The Sound of Settled Science

I'm quite certain the IPCC and the thousands of degreed researchers whose work they assess know the difference between models and observation. That deniers should have universally adopted the strategy of rejecting all models is simply evidence that none of you are interested in the truth. There is no way to investigate what will happen in the future without use of a model. Certainly, a model can be wrong but the assumption that all models are wrong and that none have value is simply bullshit.
Send in the clowns... The IPCC is a three ring circus and nothing more..
 
No matter what evidence I or anyone else have or will put up here, you will simply repeat the above bullshit mantra. AR1, 2, 3, 4 and 5 are filled with thousands of pages of observed, measured evidence supporting the AGW theory over natural variability. You are a fool and a liar. AGW is real, accepted science.

You haven't put up any evidence that supports the AGW hypothesis over natural variability...you claim that it is there but when asked for just a single piece of it, you just can't do it...because it doesn't exist.
 
I'm quite certain the IPCC and the thousands of degreed researchers whose work they assess know the difference between models and observation. That deniers should have universally adopted the strategy of rejecting all models is simply evidence that none of you are interested in the truth. There is no way to investigate what will happen in the future without use of a model. Certainly, a model can be wrong but the assumption that all models are wrong and that none have value is simply bullshit.

Funny, and pretty f'ing stupid, to be so certain when you have seen nothing like real evidence to support that certainty. The fact is, crick, that the hypothetical warming due to man's burning of hydrocarbon fuels, which is the foundation of AGW, has never actually been empirically measured, quantified and then attributed to GHG in any published, peer-reviewed scientific study to date. So exactly what is your certainty based upon?..and what might the certainty of all these "thousands" of degreed scientists be based on. Any scientists worth his degree might require some sort of actual evidence to support a hypothesis...especially a hypothesis regarding an entity as observable, and measurable as the atmosphere and radiation.
 
And, as predicted, you simply continue to lie.


Prove me wrong skid mark....lets see a single piece of observed, measured evidence that supports the AGW hypothesis over natural variability...or lets see the paper where the hypothetical warming due to man's burning of hydrocarbon fuels, which is the foundation of AGW, was empirically measured, quantified and then attributed to GHG.

You keep claiming all this evidence exists but don't seem to be able to bring any of it here. It is more than obvious that you are the liar crick..I am asking for evidence that you claim to have seen and yet, you don't seem to be able to bring it here.

We all know how much you would love to slap me down and prove that I am lying....well all you have to do is bring that one piece of evidence here, or provide a peer reviewed published paper...to prove me wrong...or you could continue your impotent, mewling, spew and yet again, show that I am, in fact, telling the truth and that you are full of shite.
 
You are an idiot, a fool and a liar.

Dozens and dozens of links to the following material and more have been provided over the past several years and yet SSDD and other simply claim it does not exist. Anyone taking SSDD and his ilk as references have been sorely misled.

http://www.climatechange2013.org/images/report/WG1AR5_ALL_FINAL.pdf, pag 159

Observations: Atmosphere and Surface

Executive Summary

The evidence of climate change from observations of the atmosphere and surface has grown significantly during recent years. At the same time new improved ways of characterizing and quantifying uncertainty have highlighted the challenges that remain for developing long-term global and regional climate quality data records. Currently, the observations of the atmosphere and surface indicate the following changes:

Atmospheric Composition
It is certain that atmospheric burdens of the well-mixed greenhouse gases (GHGs) targeted by the Kyoto Protocol increased from 2005 to 2011. The atmospheric abundance of carbon dioxide (CO2) was 390.5 ppm (390.3 to 390.7)1 in 2011; this is 40% greater than in 1750. Atmospheric nitrous oxide (N2O) was 324.2 ppb (324.0 to 324.4) in 2011 and has increased by 20% since 1750. Average annual increases in CO2 and N2O from 2005 to 2011 are comparable to those observed from 1996 to 2005. Atmospheric methane (CH4) was 1803.2 ppb (1801.2 to 1805.2) in 2011; this is 150% greater than before 1750. CH4 began increasing in 2007 after remaining nearly constant from 1999 to 2006. Hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and sulphur hexafluoride (SF6) all continue to increase relatively rapidly, but their contributions to radiative forcing are less than 1% of the total by well-mixed GHGs. {2.2.1.1}

For ozone-depleting substances (Montreal Protocol gases), it is certain that the global mean abundances of major chlorofluorocarbons (CFCs) are decreasing and HCFCs are increasing. Atmospheric burdens of major CFCs and some halons have decreased since 2005. HCFCs, which are transitional substitutes for CFCs, continue to increase, but the spatial distribution of their emissions is changing. {2.2.1.2}

Because of large variability and relatively short data records, confidence2 in stratospheric H2O vapour trends is low. Near-global satellite measurements of stratospheric water vapour show substantial variability but small net changes for 1992–2011. {2.2.2.1}

It is certain that global stratospheric ozone has declined from pre-1980 values. Most of the decline occurred prior to the mid 1990s; since then ozone has remained nearly constant at about 3.5% below the 1964–1980 level. {2.2.2.2}

Confidence is medium in large-scale increases of tropospheric ozone across the Northern Hemisphere (NH) since the 1970s Confidence is low in ozone changes across the Southern Hemisphere (SH) owing to limited measurements. It is likely3 that surface ozone trends in eastern North America and Western Europe since 2000 have levelled off or decreased and that surface ozone strongly increased in East Asia since the 1990s. Satellite and surface observations of ozone precursor gases NOx, CO, and non-methane volatile organic carbons indicate strong regional differences in trends. Most notably NO2 has likely decreased by 30 to 50% in Europe and North America and increased by more than a factor of 2 in Asia since the mid-1990s. {2.2.2.3, 2.2.2.4}

It is very likely that aerosol column amounts have declined over Europe and the eastern USA since the mid 1990s and increased over eastern and southern Asia since 2000. These shifting aerosol regional patterns have been observed by remote sensing of aerosol optical depth (AOD), a measure of total atmospheric aerosol load. Declining aerosol loads over Europe and North America are consistent with ground-based in situ monitoring of particulate mass. Confidence in satellite based global average AOD trends is low. {2.2.3}

Radiation Budgets
Satellite records of top of the atmosphere radiation fluxes have been substantially extended since AR4, and it is unlikely that significant trends exist in global and tropical radiation budgets since 2000. Interannual variability in the Earth’s energy imbalance related to El Niño-Southern Oscillation is consistent with ocean heat content records within observational uncertainty. {2.3.2}

Surface solar radiation likely underwent widespread decadal changes after 1950, with decreases (‘dimming’) until the 1980s and subsequent increases (‘brightening’) observed at many land-based sites. There is medium confidence for increasing downward thermal and net radiation at land-based observation sites since the early 1990s. {2.3.3}

Temperature

It is certain that Global Mean Surface Temperature has increased since the late 19th century. Each of the past three decades has been successively warmer at the Earth’s surface than all the previous decades in the instrumental record, and the first decade of the 21st century has been the warmest. The globally averaged combined land and ocean surface temperature data as calculated by a linear trend, show a warming of 0.85 [0.65 to 1.06] °C, over the period 1880–2012, when multiple independently produced datasets exist, and about 0.72°C [0.49°C to 0.89°C] over the period 1951–2012. The total increase between the average of the 1850–1900 period and the 2003– 2012 period is 0.78 [0.72 to 0.85] °C and the total increase between the average of the 1850–1900 period and the reference period for projections, 1986−2005, is 0.61 [0.55 to 0.67] °C, based on the single longest dataset available. For the longest period when calculation of regional trends is sufficiently complete (1901–2012), almost the entire globe has experienced surface warming. In addition to robust multidecadal warming, global mean surface temperature exhibits substantial decadal and interannual variability. Owing to natural variability, trends based on short records are very sensitive to the beginning and end dates and do not in general reflect long-term climate trends. As one example, the rate of warming over the past 15 years (1998–2012; 0.05 [–0.05 to +0.15] °C per decade), which begins with a strong El Niño, is smaller than the rate calculated since 1951 (1951–2012; 0.12 [0.08 to 0.14] °C per decade). Trends for 15-year periods starting in 1995, 1996, and 1997 are 0.13 [0.02 to 0.24], 0.14 [0.03 to 0.24] and 0.07 [–0.02 to 0.18], respectively. Several independently analyzed data records of global and regional land-surface air temperature (LSAT) obtained from station observations are in broad agreement that LSAT has increased. Sea surface temperatures (SSTs) have also increased. Intercomparisons of new SST data records obtained by different measurement methods, including satellite data, have resulted in better understanding of uncertainties and biases in the records. {2.4.1, 2.4.2, 2.4.3; Box 9.2}

It is unlikely that any uncorrected urban heat-island effects and land use change effects have raised the estimated centennial globally averaged LSAT trends by more than 10% of the reported trend. This is an average value; in some regions with rapid development, urban heat island and land use change impacts on regional trends may be substantially larger. {2.4.1.3}

Confidence is medium in reported decreases in observed global diurnal temperature range (DTR), noted as a key uncertainty in the AR4. Several recent analyses of the raw data on which many previous analyses were based point to the potential for biases that differently affect maximum and minimum average temperatures. However, apparent changes in DTR are much smaller than reported changes in average temperatures and therefore it is virtually certain that maximum and minimum temperatures have increased since 1950. {2.4.1.2}

Based on multiple independent analyses of measurements from radiosondes and satellite sensors it is virtually certain that globally the troposphere has warmed and the stratosphere has cooled since the mid-20th century. Despite unanimous agreement on the sign of the trends, substantial disagreement exists among available estimates as to the rate of temperature changes, particularly outside the NH extratropical troposphere, which has been well sampled by radiosondes. Hence there is only medium confidence in the rate of change and its vertical structure in the NH extratropical troposphere and low confidence elsewhere. {2.4.4}

Hydrological Cycle
Confidence in precipitation change averaged over global land areas since 1901 is low for years prior to 1951 and medium afterwards. Averaged over the mid-latitude land areas of the Northern Hemisphere, precipitation has likely increased since 1901 (medium confidence before and high confidence after 1951). For other latitudinal zones area-averaged long-term positive or negative trends have low confidence due to data quality, data completeness or disagreement amongst available estimates. {2.5.1.1, 2.5.1.2}

It is very likely that global near surface and tropospheric air specific humidity have increased since the 1970s. However, during recent years the near surface moistening over land has abated (medium confidence). As a result, fairly widespread decreases in relative humidity near the surface are observed over the land in recent years. {2.4.4, 2.5.4, 2.5.5}

While trends of cloud cover are consistent between independent data sets in certain regions, substantial ambiguity and therefore low confidence remains in the observations of global-scale cloud variability and trends. {2.5.6}

Extreme Events
It is very likely that the numbers of cold days and nights have decreased and the numbers of warm days and nights have increased globally since about 1950. There is only medium confidence that the length and frequency of warm spells, including heat waves, has increased since the middle of the 20th century mostly owing to lack of data or of studies in Africa and South America. However, it is likely that heatwave frequency has increased during this period in large parts of Europe, Asia and Australia. {2.6.1}

It is likely that since about 1950 the number of heavy precipitation events over land has increased in more regions than it has decreased. Confidence is highest for North America and Europe where there have been likely increases in either the frequency or intensity of heavy precipitation with some seasonal and/or regional variation. It is very likely that there have been trends towards heavier precipitation events in central North America. {2.6.2.1}

Confidence is low for a global-scale observed trend in drought or dryness (lack of rainfall) since the middle of the 20th century, owing to lack of direct observations, methodological uncertainties and geographical inconsistencies in the trends. Based on updated studies, AR4 conclusions regarding global increasing trends in drought since the 1970s were probably overstated. However, this masks important regional changes: the frequency and intensity of drought have likely increased in the Mediterranean and West Africa and likely decreased in central North America and north-west Australia since 1950. {2.6.2.2}

Confidence remains low for long-term (centennial) changes in tropical cyclone activity, after accounting for past changes in observing capabilities. However, it is virtually certain that the frequency and intensity of the strongest tropical cyclones in the North Atlantic has increased since the 1970s. {2.6.3}

Confidence in large-scale trends in storminess or storminess proxies over the last century is low owing to inconsistencies
between studies or lack of long-term data in some parts of the world (particularly in the SH). {2.6.4}

Because of insufficient studies and data quality issues confidence is also low for trends in small-scale severe weather events such as hail or thunderstorms. {2.6.2.4}

Atmospheric Circulation and Indices of Variability

It is likely that circulation features have moved poleward since the 1970s, involving a widening of the tropical belt, a poleward shift of storm tracks and jet streams, and a contraction of the northern polar vortex. Evidence is more robust for the NH. It is likely that the Southern Annular Mode has become more positive since the 1950s. {2.7.5, 2.7.6, 2.7.8; Box 2.5}

Large variability on interannual to decadal time scales hampers robust conclusions on long-term changes in atmospheric circulation in many instances. Confidence is high that the increase in the northern mid-latitude westerly winds and the North Atlantic Oscillation (NAO) index from the 1950s to the 1990s and the weakening of the Pacific Walker circulation from the late 19th century to the 1990s have been largely offset by recent changes. {2.7.5, 2.7.8, Box 2.5}

Confidence in the existence of long-term changes in remaining aspects of the global circulation is low owing to observational limitations or limited understanding. These include surface winds over land, the East Asian summer monsoon circulation, the tropical cold-point tropopause temperature and the strength of the Brewer Dobson circulation. {2.7.2, 2.7.4, 2.7.5, 2.7.7}
 
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Observations: Ocean

Executive Summary

Temperature and Heat Content Changes

It is virtually certain1 that the upper ocean (above 700 m) has warmed from 1971 to 2010, and likely that it has warmed from the 1870s to 1971. Confidence in the assessment for the time period since 1971 is high2 based on increased data coverage after this date and on a high level of agreement among independent observations of subsurface temperature [3.2], sea surface temperature [2.4.2], and sea level rise, which is known to include a substantial component due to thermal expansion [3.7, Chapter 13]. There is less certainty in changes prior to 1971 because of relatively sparse sampling in earlier time periods. The strongest warming is found near the sea surface (0.11 [0.09 to 0.13] °C per decade in the upper 75 m between 1971 and 2010), decreasing to about 0.015°C per decade at 700 m. It is very likely that the surface intensification of this warming signal increased the thermal stratification of the upper ocean by about 4% between 0 and 200 m depth. Instrumental biases in historical upper ocean temperature measurements have been identified and reduced since AR4, diminishing artificial decadal variation in temperature and upper ocean heat content, most prominent during the 1970s and 1980s. {3.2.1–3.2.3, Figures 3.1, 3.2 and 3.9}

It is likely that the ocean warmed between 700 and 2000 m from 1957 to 2009, based on 5-year averages. It is likely that the ocean warmed from 3000 m to the bottom from 1992 to 2005, while no significant trends in global average temperature were observed between 2000 and 3000 m depth during this period. Warming below 3000 m is largest in the Southern Ocean {3.2.4, 3.5.1, Figures 3.2b and 3.3, FAQ 3.1}

It is virtually certain that upper ocean (0 to 700 m) heat content increased during the relatively well-sampled 40-year period from 1971 to 2010. Published rates for that time period range from 74 TW to 137 TW, with generally smaller trends for estimates that assume zero anomalies in regions with sparse data. Using a statistical analysis of ocean variability to estimate change in sparsely sampled areas and to estimate uncertainties results in a rate of increase of global upper ocean heat content of 137 [120–154] TW (medium confidence). Although not all trends agree within their statistical uncertainties, all are positive, and all are statistically different from zero. {3.2.3, Figure 3.2}

Warming of the ocean between 700 and 2000 m likely contributed about 30% of the total increase in global ocean heat content (0 to 2000 m) between 1957 and 2009. Although globally
integrated ocean heat content in some of the 0 to 700 m estimates increased more slowly from 2003 to 2010 than over the previous decade, ocean heat uptake from 700 to 2000 m likely continued unabated during this period. {3.2.4, Figure 3.2, Box 9.2}

Ocean warming dominates the global energy change inventory. Warming of the ocean accounts for about 93% of the increase in the Earth’s energy inventory between 1971 and 2010 (high confidence), with warming of the upper (0 to 700 m) ocean accounting for about 64% of the total. Melting ice (including Arctic sea ice, ice sheets and glaciers) and warming of the continents and atmosphere account for the remainder of the change in energy. The estimated net increase in the Earth’s energy storage between 1971 and 2010 is 274 [196 to 351] ZJ (1 ZJ = 1021 Joules), with a heating rate of 213 TW from a linear fit to annual inventories over that time period, equivalent to 0.42 W m–2 heating applied continuously over the Earth’s entire surface, and 0.55 W m–2 for the portion due to ocean warming applied over the ocean surface area. {Section 3.2.3, Figure 3.2, Box 3.1}

Salinity and Freshwater Content Changes

It is very likely that regional trends have enhanced the mean geographical contrasts in sea surface salinity since the 1950s: saline surface waters in the evaporation-dominated midlatitudes have become more saline, while relatively fresh surface waters in rainfall-dominated tropical and polar regions have become fresher. The mean contrast between high- and lowsalinity regions increased by 0.13 [0.08 to 0.17] from 1950 to 2008. It is very likely that the interbasin contrast in freshwater content has increased: the Atlantic has become saltier and the Pacific and Southern oceans have freshened. Although similar conclusions were reached in AR4, recent studies based on expanded data sets and new analysis approaches provide high confidence in the assessment of trends in ocean salinity. {3.3.2, 3.3.3, 3.3.5, Figures 3.4, 3.5 and 3.21d, FAQ 3.2}

It is very likely that large-scale trends in salinity have also occurred in the ocean interior. It is likely that both the subduction of surface water anomalies formed by changes in evaporation – precipitation (E – P) and the movement of density surfaces due to warming have contributed to the observed changes in subsurface salinity. {3.3.2–3.3.4, Figures 3.5 and 3.9}

The spatial patterns of the salinity trends, mean salinity and the mean distribution of E – P are all similar. This provides, with medium confidence, indirect evidence that the pattern of E – P over the oceans has been enhanced since the 1950s. {3.3.2–3.3.4, Figures 3.4, 3.5 and 3.20d, FAQ 3.2}.

Air–Sea Flux and Wave Height Changes

Uncertainties in air–sea heat flux data sets are too large to allow detection of the change in global mean net air-sea heat flux, of the order of 0.5 W m–2 since 1971, required for consistency with the observed ocean heat content increase. The products cannot yet be reliably used to directly identify trends in the regional or global distribution of evaporation or precipitation over the oceans on the time scale of the observed salinity changes since 1950. {3.4.2, 3.4.3, Figures 3.6 and 3.7}

Basin-scale wind stress trends at decadal to centennial time scales have been observed in the North Atlantic, Tropical Pacific and Southern Ocean with low to medium confidence. These results are based largely on atmospheric reanalyses, in some cases a single product, and the confidence level is dependent on region and time scale considered. The evidence is strongest for the Southern Ocean, for which there is medium confidence that zonal mean wind stress has increased in strength since the early 1980s. {3.4.4, Figure 3.8}

There is medium confidence based on ship observations and reanalysis forced wave model hindcasts that mean significant wave height has increased since the 1950s over much of the North Atlantic north of 45°N, with typical winter season trends of up to 20 cm per decade. {3.4.5}

Changes in Water Masses and Circulation

Observed changes in water mass properties likely reflect the combined effect of long-term trends in surface forcing (e.g., warming of the surface ocean and changes in E – P) and interannual-to-multi-decadal variability related to climate modes. Most of the observed temperature and salinity changes in the ocean interior can be explained by subduction and spreading of water masses with properties that have been modified at the sea surface. From 1950 to 2000, it is likely that subtropical salinity maximum waters became more saline, while fresh intermediate waters formed at higher latitude have generally become fresher. For Upper North Atlantic Deep Water changes in properties and formation rates are very likely dominated by decadal variability. The Lower North Atlantic Deep Water has likely cooled from 1955 to 2005, and the freshening trend highlighted in AR4 reversed in the mid-1990s. It is likely that the Antarctic Bottom Water warmed and contracted globally since the 1980s and freshened in the Indian/Pacific sectors from 1970 to 2008. {3.5, FAQ 3.1}

Recent observations have strengthened evidence for variability in major ocean circulation systems on time scales from years to decades. It is very likely that the subtropical gyres in the North Pacific and South Pacific have expanded and strengthened since 1993. It is about as likely as not that this is linked to decadal variability in wind forcing rather than being part of a longer-term trend. Based on measurements of the full Atlantic Meridional Overturning Circulation and its individual components at various latitudes and different time periods, there is no evidence of a long-term trend. There is also no evidence for trends in the transports of the Indonesian Throughflow, the AntarcticCircumpolar Current (ACC), or between the Atlantic Ocean and Nordic Seas. However, there is medium confidence that the ACC shifted south between 1950 and 2010, at a rate equivalent to about 1° of latitude in 40 years. {3.6, Figures 3.10, 3.11}

Sea Level Change

Global mean sea level (GMSL) has risen by 0.19 [0.17 to 0.21] m over the period 1901–2010, calculated using the mean rate over these 110 years, based on tide gauge records and since 1993 additionally on satellite data. It is very likely that the mean rate was 1.7 [1.5 to 1.9] mm yr–1 between 1901 and 2010 and increased to 3.2 [2.8 to 3.6] mm yr–1 between 1993 and 2010. This assessment is based on high agreement among multiple studies using different methods, long tide gauge records corrected for vertical land motion and independent observing systems (tide gauges and altimetry) since 1993 (see also TFE.2, Figure 1). It is likely that GMSL rose between 1920 and 1950 at a rate comparable to that observed between 1993 and 2010, as individual tide gauges around the world and reconstructions of GMSL show increased rates of sea level rise during this period. Rates of sea level rise over broad regions can be several times larger or smaller than that of GMSL for periods of several decades due to fluctuations in ocean circulation. High agreement between studies with and without corrections for vertical land motion suggests that it is very unlikely that estimates of the global average rate of sea level change are significantly biased owing to vertical land motion that has been unaccounted for. {3.7.2, 3.7.3, Table 3.1, Figures 3.12, 3.13, 3.14}

It is very likely that warming of the upper 700 m has been contributing an average of 0.6 [0.4 to 0.8] mm yr–1 of sea level rise since 1971. It is likely that warming between 700 m and 2000 m has been contributing an additional 0.1 mm yr–1 [0 to 0.2] of sea level rise since 1971, and that warming below 2000 m has been contributing another 0.1 [0.0 to 0.2] mm yr–1 of sea level rise since the early 1990s. {3.7.2, Figure 3.13}

It is likely that the rate of sea level rise increased from the early 19th century to the early 20th century, and increased further over the 20th century. The inference of 19th century change is based on a small number of very long tide gauge records from northern Europe and North America. Multiple long tide gauge records and reconstructions of global mean sea level confirm a higher rate of rise from the late 19th century. It is likely that the average acceleration over the 20th century is [–0.002 to 0.019] mm yr–2, as two of three reconstructions extending back to at least 1900 show an acceleration during the 20th century. {3.7.4}

It is likely that the magnitude of extreme high sea level events has increased since 1970. A rise in mean sea level can explain most of the increase in extreme sea levels: changes in extreme high sea levels are reduced to less than 5 mm yr–1 at 94% of tide gauges once the rise in mean sea level is accounted for. {3.7.5, Figure 3.15}

Changes in Ocean Biogeochemistry

Based on high agreement between independent estimates using different methods and data sets (e.g., oceanic carbon, oxygen, and transient tracer data), it is very likely that the global ocean inventory of anthropogenic carbon (Cant ) increased from 1994 to 2010 . The oceanic Cant inventory in 2010 is estimated to be 155 PgC with an uncertainty of ±20%. The annual global oceanic uptake rates calculated from independent data sets (from oceanic Cant inventory changes, from atmospheric O 2/N 2 measurements or from partial pressure of carbon dioxide (pCO 2) data) and for different time periods agree with each other within their uncertainties and very likely are in the range of 1.0 to 3.2 PgC yr–1 {3.8.1, Figure 3.16}

Uptake of anthropogenic CO2 results in gradual acidification of the ocean. The pH of surface seawater has decreased by 0.1 since the beginning of the industrial era, corresponding to a 26% increase in hydrogen ion concentration (high confidence). The observed pH trends range between –0.0014 and –0.0024 yr–1 in surface waters. In the ocean interior, natural physical and biological processes, as well as uptake of anthropogenic CO 2 , can cause changes in pH over decadal and longer time scales. {3.8.2, Table 3.2, Box 3.2, Figures 3.18, 3.19, FAQ 3.3}

High agreement among analyses provides medium confidence that oxygen concentrations have decreased in the open ocean thermocline in many ocean regions since the 1960s. The general decline is consistent with the expectation that warming-induced stratification leads to a decrease in the supply of oxygen to the thermocline from near surface waters, that warmer waters can hold less oxygen, and that changes in wind-driven circulation affect oxygen concentra - tions. It is likely that the tropical oxygen minimum zones have expand - ed in recent decades. {3.8.3, Figure 3.20}

Synthesis

The observations summarized in this chapter provide strong evidence that ocean properties of relevance to climate have changed during the past 40 years, including temperature, salinity, sea level, carbon, pH, and oxygen. The observed patterns of change in the subsurface ocean are consistent with changes in the surface ocean in response to climate change and natural variability and with known physical and biogeochemical processes in the ocean, providing high confidence in this assessment. {3.9, Figures 3.21, 3.22}
 
Send in the clowns... The IPCC is a three ring circus and nothing more..

Here -in two parts - are the references - the published, peer-reviewed empirical studies on which only Chapter 2, "Observations: Surface and Atmosphere" of Working Group I's report: "The Physical Science Basis" is based. If I hear more crap like the line above or SSDD's charge that such data do not exist, I will give you the references for Chapter 3.

References Abakumova, G. M., E. V. Gorbarenko, E. I. Nezval, and O. A. Shilovtseva, 2008: Fifty years of actinometrical measurements in Moscow. Int. J. Remote Sens., 29, 2629–2665. Adam, J. C., and D. P. Lettenmaier, 2008: Application of new precipitation and reconstructed streamflow products to streamflow trend attribution in northern Eurasia. J. Clim., 21, 1807–1828. Adler, R. F., G. J. Gu, and G. J. Huffman, 2012: Estimating climatological bias errors for the global Precipitation Climatology Project (GPCP). J. Appl. Meteor. Climatol., 51, 84–99. Adler, R. F., et al., 2003: The version-2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present). J. Hydrometeor., 4, 1147–1167. Aguilar, E., et al., 2009: Changes in temperature and precipitation extremes in western central Africa, Guinea Conakry, and Zimbabwe, 1955–2006. J. Geophys. Res. Atmos., 114, D02115. Alexander, L. V., P. Uotila, and N. Nicholls, 2009: Influence of sea surface temperature variability on global temperature and precipitation extremes. J. Geophys. Res. Atmos., 114, D18116. Alexander, L. V., X. L. L. Wang, H. Wan, and B. Trewin, 2011: Significant decline in storminess over southeast Australia since the late 19th century. Aust. Meteor. Ocean. J., 61, 23–30. Alexander, L. V., et al., 2006: Global observed changes in daily climate extremes of temperature and precipitation. J. Geophys. Res. Atmos., 111, D05109. Allan, R., and T. Ansell, 2006: A new globally complete monthly historical gridded mean sea level pressure dataset (HadSLP2): 1850–2004. J. Clim., 19, 5816–5842. Allan, R., S. Tett, and L. Alexander, 2009: Fluctuations in autumn-winter severe storms over the British Isles: 1920 to present. Int. J. Climatol., 29, 357–371. Allan, R. P., 2009: Examination of relationships between clear-sky longwave radiation and aspects of the atmospheric hydrological cycle in climate models, reanalyses, and observations. J. Clim., 22, 3127–3145. Allan, R. P., and A. Slingo, 2002: Can current climate model forcings explain the spatial and temporal signatures of decadal OLR variations? Geophys. Res. Lett., 29, 1141. Allan, R. P., and B. J. Soden, 2008: Atmospheric warming and the amplification of precipitation extremes. Science, 321, 1481–1484. Allan, R. P., B. J. Soden, V. O. John, W. Ingram, and P. Good, 2010: Current changes in tropical precipitation. Environ. Res. Lett., 5, 025205. Allen, R. J., and S. C. Sherwood, 2007: Utility of radiosonde wind data in representing climatological variations of tropospheric temperature and baroclinicity in the western tropical Pacific. J. Clim., 20, 5229–5243. Allen, R. J., and S. C. Sherwood, 2008: Warming maximum in the tropical upper troposphere deduced from thermal winds. Nature Geosci., 1, 399–403. Alpert, P., and P. Kishcha, 2008: Quantification of the effect of urbanization on solar dimming. Geophys. Res. Lett., 35, L08801. Alpert, P., P. Kishcha, Y. J. Kaufman, and R. Schwarzbard, 2005: Global dimming or local dimming? Effect of urbanization on sunlight availability. Geophys. Res. Lett., 32, L17802. Andrade, C., S. Leite, and J. Santos, 2012: Temperature extremes in Europe: Overview of their driving atmospheric patterns. Nat. Hazards Earth Syst. Sci., 12, 1671–1691. Andronova, N., J. E. Penner, and T. Wong, 2009: Observed and modeled evolution of the tropical mean radiation budget at the top of the atmosphere since 1985. J. Geophys. Res. Atmos., 114, D14106. Angell, J. K., 2006: Changes in the 300-mb North Circumpolar Vortex, 1963–2001. J. Clim., 19, 2984–2994. Anthes, R. A., 2011: Exploring Earth’s atmosphere with radio occultation: contributions to weather, climate and space weather. Atmos. Meas. Tech., 4, 1077–1103. Anthes, R. A., et al., 2008: The COSMOC/FORMOSAT-3 Mission—Early results. Bull. Am. Meteor. Soc., 89, 313. Archer, C. L., and K. Caldeira, 2008a: Reply to comment by Courtenay Strong and Robert E. Davis on “Historical trends in the jet streams”. Geophys. Res. Lett., 35. L24807. Archer, C. L., and K. Caldeira, 2008b: Historical trends in the jet streams. Geophys. Res. Lett., 35, L08803. Arndt, D. S., M. O. Baringer, and M. R. Johnson, 2010: State of the Climate in 2009. Bull. Am. Meteor. Soc., 91, S1–. Arnold, T., et al., 2013: Nitrogen trifluoride global emissions estimated from updated atmospheric measurements. Proc. Natl. Acad. Sci. U.S.A., 110, 2029–2034. Ashok, K., S. K. Behera, S. A. Rao, H. Y. Weng, and T. Yamagata, 2007: El Niño Modoki and its possible teleconnection. J. Geophys. Res. Oceans, 112, C11007. Asmi, A., et al., 2013: Aerosol decadal trends – Part 2: In-situ aerosol particle number concentrations at GAW and ACTRIS stations. Atmos. Chem. Phys., 13, 895–916. Atlas, R., R. Hoffman, J. Ardizzone, S. Leidner, J. Jusem, D. Smith, and D. Gombos, 2011: A cross-calibrated mutiplatform ocean wind velocity product for meteorlogical and oceanographic applications. Bull. Am. Meteor. Soc., 92, 157–. Augustine, J. A., and E. G. Dutton, 2013: Variability of the surface radiation budget over United States from 1996 through 2011 from high-quality measurements. J. Geophys. Res., 118, 43-53, Aydin, M., et al., 2011: Recent decreases in fossil-fuel emissions of ethane and methane derived from firn air. Nature, 476, 198–201. Ballester, J., F. Giorgi, and X. Rodo, 2010: Changes in European temperature extremes can be predicted from changes in PDF central statistics. Clim. Change, 98, 277– 284. Baringer, M. O., D. S. Arndt, and M. R. Johnson, 2010: State of the Climate in 2009. Bull. Am. Meteor. Soc., 91, S1–. Barmpadimos, I., J. Keller, D. Oderbolz, C. Hueglin, and A. S. H. Prévôt, 2012: One decade of parallel fine (PM2.5) and coarse (PM10–PM2.5) particulate matter measurements in Europe: trends and variability. Atmos. Chem. Phys., 12, 3189– 3203. Barnston, A. G., and R. E. Livezey, 1987: Classification, seasonality and persistence of low-frequency atmospheric circulation patterns. Mon. Weather Rev., 115, 1083–1126. Barring, L., and K. Fortuniak, 2009: Multi-indices analysis of southern Scandinavian storminess 1780–2005 and links to interdecadal variations in the NW EuropeNorth Sea region. Int. J. Climatol., 29, 373–384. Barriopedro, D., E. M. Fischer, J. Luterbacher, R. Trigo, and R. Garcia-Herrera, 2011: The hot summer of 2010: Redrawing the temperature record map of Europe. Science, 332, 220–224. Barrucand, M., M. Rusticucci, and W. Vargas, 2008: Temperature extremes in the south of South America in relation to Atlantic Ocean surface temperature and Southern Hemisphere circulation. J. Geophys. Res. Atmos., 113, D20111. Barton, N. P., and A. W. Ellis, 2009: Variability in wintertime position and strength of the North Pacific jet stream as represented by re-analysis data. Int. J. Climatol., 29, 851–862. Becker, A., et al., 2013: A description of the global land-surface precipitation data products of the Global Precipitation Climatology Centre with sample applications including centennial (trend) analysis from 1901–present. Earth Syst. Sci. Data, 5, 71–99. Beig, G., and V. Singh, 2007: Trends in tropical tropospheric column ozone from satellite data and MOZART model. Geophys. Res. Lett., 34, L17801. Bell, G. D., and M. S. Halpert, 1998: Climate assessment for 1997. Bull. Am. Meteor. Soc., 79, S1–S50. Bender, F. A. M., V. Ramanathan, and G. Tselioudis, 2012: Changes in extratropical storm track cloudiness 1983–2008: Observational support for a poleward shift. Clim. Dyn., 38, 2037–2053. Bengtsson, L., and K. I. Hodges, 2011: On the evaluation of temperature trends in the tropical troposphere. Clim. Dyn., 36, 419–430. Beniston, M., 2004: The 2003 heat wave in Europe: A shape of things to come? An analysis based on Swiss climatological data and model simulations. Geophys. Res. Lett., 31, L02202. Beniston, M., 2009: Decadal-scale changes in the tails of probability distribution functions of climate variables in Switzerland. Int. J. Climatol., 29, 1362–1368. Bennartz, R., J. Fan, J. Rausch, L. Leung, and A. Heidinger, 2011: Pollution from China increases cloud droplet number, suppresses rain over the East China Sea. Geophys. Res. Lett., 38, L09704. Berrisford, P., et al., 2011: Atmospheric conservation properties in ERA-Interim. Q. J. R. Meteor. Soc., 137, 1381–1399. Berry, D., and E. Kent, 2011: Air-Sea fluxes from ICOADS: The construction of a new gridded dataset with uncertainty estimates. Int. J. Climatol., 31, 987–1001. Berry, D. I., and E. C. Kent, 2009: A new air-sea interaction gridded dataset from ICOADS with uncertainty estimates. Bull. Am. Meteor. Soc., 90, 645-656. Berthet, C., J. Dessens, and J. Sanchez, 2011: Regional and yearly variations of hail frequency and intensity in France. Atmos. Res., 100, 391–400. Birner, T., 2010: Recent widening of the tropical belt from global tropopause statistics: Sensitivities. J. Geophys. Res. Atmos., 115, D23109. Bitz, C. M., and Q. Fu, 2008: Arctic warming aloft is data set dependent. Nature, 455, E3–E4. Black, E., and R. Sutton, 2007: The influence of oceanic conditions on the hot European summer of 2003. Clim. Dyn., 28, 53–66. Blunden, J., D. S. Arndt, and M. O. Baringer, 2011: State of the Climate in 2010. Bull. Am. Meteor. Soc., 92, S17–. Bohm, R., P. D. Jones, J. Hiebl, D. Frank, M. Brunetti, and M. Maugeri, 2010: The early instrumental warm-bias: A solution for long central European temperature series 1760–2007. Clim. Change, 101, 41–67. Bonfils, C., P. B. Duffy, B. D. Santer, T. M. L. Wigley, D. B. Lobell, T. J. Phillips, and C. Doutriaux, 2008: Identification of external influences on temperatures in California. Clim. Change, 87, S43–S55. Bonisch, H., A. Engel, J. Curtius, T. Birner, and P. Hoor, 2009: Quantifying transport into the lowermost stratosphere using simultaneous in-situ measurements of SF6 and CO2. Atmos. Chem. Phys., 9, 5905–5919. Bosilovich, M. G., F. R. Robertson, and J. Chen, 2011: Global energy and water budgets in MERRA. J. Clim., 24, 5721-5739.. Bourassa, M. A., S. T. Gille, D. L. Jackson, J. B. Roberts, and G. A. Wick, 2010: Ocean winds and turbulent air-sea fluxes inferred from remote sensing. Oceanography, 23, 36–51. Bousquet, P., 2011: Source attribution of the changes in atmospheric methane for 2006–2008. Atmos. Chem. Phys. Discuss., 10, 27603–27630. Brogniez, H., R. Roca, and L. Picon, 2009: Study of the free tropospheric humidity interannual variability using meteosat data and an advection-condensation transport model. J. Clim., 22, 6773–6787. Brönnimann, S., 2009: Early twentieth-century warming. Nature Geosci., 2, 735–736. Brönnimann, S., et al., 2009: Variability of large-scale atmospheric circulation indices for the Northern Hemisphere during the past 100 years. Meteorol. Z., 18, 379–396. Brooks, C. F., 1926: Observing water-surface temperatures at sea. Mon. Wea. Rev., 54, 241–253. Brooks, H., 2012: Severe thunderstorms and climate change. Atmos. Res., 123, SI, 129-138. Brooks, H. E., and N. Dotzek, 2008: The spatial distribution of severe convective storms and an analysis of their secular changes. In: Climate Extremes and Society [H. F. Diaz and R. J. Murnane (eds.] Cambridge University Press, pp. 35–53. Brown, S. J., J. Caesar, and C. A. T. Ferro, 2008: Global changes in extreme daily temperature since 1950. J. Geophys. Res. Atmos., 113, D05115. Brunet, M., et al., 2011: The minimization of the screen bias from ancient Western Mediterranean air temperature records: an exploratory statistical analysis. Int. J. Climatol., 31, 1879–1895. Bunge, L., and A. J. Clarke, 2009: A verified estimation of the El Niño Index Niño-3.4 since 1877. J. Clim., 22, 3979–3992. Burn, D. H., and N. M. Hesch, 2007: Trends in evaporation for the Canadian prairies. J. Hydrol., 336, 61–73. Caesar, J., L. Alexander, and R. Vose, 2006: Large-scale changes in observed daily maximum and minimum temperatures: Creation and analysis of a new gridded data set. J. Geophys. Res. Atmos., 111, D05101. Caesar, J., et al., 2011: Changes in temperature and precipitation extremes over the Indo-Pacific region from 1971 to 2005. Int. J. Climatol., 31, 791–801. Cai, W., and P. van Rensch, 2012: The 2011 southeast Queensland extreme summer rainfall: A confirmation of a negative Pacific Decadal Oscillation phase? Geophys. Res. Lett., 39, L08702. Cai, W., T. Cowan, and M. Thatcher, 2012: Rainfall reductions over Southern Hemisphere semi-arid regions: The role of subtropical dry zone expansion. Sci. Rep., 2, 702. Callaghan, J., and S. B. Power, 2011: Variability and decline in the number of severe tropical cyclones making land-fall over eastern Australia since the late nineteenth century. Clim. Dyn., 37, 647–662. Canada, 2012: Canadian Smog Science Assessment – Highlights and Key Messages. Environment Canada and Health Canada, 64 pp. Cane, M. A., 1986: El-Niño. Annu. Rev. Earth Planet. Sci., 14, 43–70. Cao, Z. H., 2008: Severe hail frequency over Ontario, Canada: Recent trend and variability. Geophys. Res. Lett., 35. L14803. Carslaw, K. S., O. Boucher, D. Spracklen, G. Mann, J. G. Rae, S. Woodward, and M. Kumala, 2010: A review of natural aerosol interactions and feedbacks within the Earth system. Atmos. Chem. Phys., 10, 1701–1737. Casey, K. S., T. B. Brandon, P. Cornillon, and R. Evans, 2010: The past, present and future of the AVHRR Pathfinder SST Program. In: Oceanography from Space: Revisited [V. Barale, J. F. R. Gower, and L. Alberotanza (eds.)]. Springer Science+Business Media, New York, 323-341. Castellanos, P., and K. F. Boersma, 2012: Reductions in nitrogen oxides over Europe driven by environmental policy and economic recession. Sci. Rep., 2. 265. Cermak, J., M. Wild, R. Knutti, M. I. Mishchenko, and A. K. Heidinger, 2010: Consistency of global satellite-derived aerosol and cloud data sets with recent brightening observations. Geophys. Res. Lett., 37, L21704. Chambers, L., and G. Griffiths, 2008: The changing nature of temperature extremes in Australia and New Zealand. Aust. Meteorol. Mag., 57, 13–35. Chan, J. C. L., and M. Xu, 2009: Inter-annual and inter-decadal variations of landfalling tropical cyclones in East Asia. Part I: time series analysis. Int. J. Climatol., 29, 1285–1293. Chandler, R. E., and E. M. Scott, 2011: Statistical Methods for Trend Detection and Analysis in the Environmental Sciences. John Wiley & Sons, Hoboken, NJ. Chang, E. K. M., 2007: Assessing the increasing trend in Northern Hemisphere winter storm track activity using surface ship observations and a statistical storm track model. J. Clim., 20, 5607–5628. Chang, E. K. M., and Y. J. Guo, 2007: Is the number of North Atlantic tropical cyclones significantly underestimated prior to the availability of satellite observations? Geophys. Res. Lett., 34. L14801. Chapman, W. L., and J. E. Walsh, 2007: A synthesis of Antarctic temperatures. J. Clim., 20, 4096–4117. Che, H. Z., et al., 2005: Analysis of 40 years of solar radiation data from China, 1961–2000. Geophys. Res. Lett., 32, L06803. Chen, J. Y., B. E. Carlson, and A. D. Del Genio, 2002: Evidence for strengthening of the tropical general circulation in the 1990s. Science, 295, 838–841. Chen, J. Y., A. D. Del Genio, B. E. Carlson, and M. G. Bosilovich, 2008: The spatiotemporal structure of twentieth-century climate variations in observations and reanalyses. Part I: Long-term trend. J. Clim., 21, 2611–2633. Chiacchio, M., and M. Wild, 2010: Influence of NAO and clouds on long-term seasonal variations of surface solar radiation in Europe. J. Geophys. Res. Atmos., 115, D00d22. Choi, G., et al., 2009: Changes in means and extreme events of temperature and precipitation in the Asia Pacific Network region, 1955–2007. Int. J. Climatol., 29, 1906–1925. Christy, J. R., and W. B. Norris, 2006: Satellite and VIZ-radiosonde intercomparisons for diagnosis of nonclimatic influences. J. Atmos. Ocean. Technol., 23, 1181– 1194. Christy, J. R., and W. B. Norris, 2009: Discontinuity issues with radiosonde and satellite temperatures in the Australian Region 1979–2006. J. Atmos. Ocean Technol., 26, 508–522. Christy, J. R., W. B. Norris, and R. T. McNider, 2009: Surface temperature variations in East Africa and possible causes. J. Clim., 22, 3342–3356. Christy, J. R., R. W. Spencer, and W. B. Norris, 2011: The role of remote sensing in monitoring global bulk tropospheric temperatures. Int. J. Remote Sens., 32, 671–685. Christy, J. R., W. B. Norris, K. Redmond, and K. P. Gallo, 2006: Methodology and results of calculating central california surface temperature trends: Evidence of human-induced climate change? J. Clim., 19, 548–563. Christy, J. R., W. B. Norris, R. W. Spencer, and J. J. Hnilo, 2007: Tropospheric temperature change since 1979 from ,tropical radiosonde and satellite measurements. J. Geophys. Res. Atmos., 112, D06102. Christy, J. R., R. W. Spencer, W. B. Norris, W. D. Braswell, and D. E. Parker, 2003: Error estimates of version 5.0 of MSU-AMSU bulk atmospheric temperatures. J. Atmos. Ocean Technol., 20, 613–629. Christy, J. R., et al., 2010: What do observational datasets say about modeled tropospheric temperature trends since 1979? , 2148–2169. Chu, W. P., M. P. McCormick, J. Lenoble, C. Brogniez, and P. Pruvost, 1989: SAGE II inversion algorithm. J. Geophys. Res. Atmos., 94, 8339–8351. Chung, E. S., and B. J. Soden, 2010: Investigating the influence of carbon dioxide and the stratosphere on the long-term tropospheric temperature monitoring from HIRS. J. Appl. Meteor. Climatol., 49, 1927–1937 Chung, E. S., D. Yeomans, and B. J. Soden, 2010: An assessment of climate feedback processes using satellite observations of clear-sky OLR. Geophys. Res. Lett., 37, L02702. Clark, R. T., S. J. Brown, and J. M. Murphy, 2006: Modeling Northern Hemisphere summer heat extreme changes and their uncertainties using a physics ensemble of climate sensitivity experiments. J. Clim., 19, 4418–4435. Clement, A. C., and B. Soden, 2005: The sensitivity of the tropical-mean radiation budget. J. Clim., 18, 3189–3203. CMA, 2007: Atlas of China Disastrous Weather and Climate. Chinese Meteorological Administration. Beijing, China. CMA, 2011: China Climate Change Bulletin. Chinese Meteorological Administration. Beijing, China. Cohen, J., M. Barlow, and K. Saito, 2009: Decadal fluctuations in planetary wave forcing modulate global warming in late boreal winter. J. Clim., 22, 4418–4426. Cohen, J. L., J. C. Furtado, M. Barlow, V. A. Alexeev, and J. E. Cherry, 2012: Asymmetric seasonal temperature trends. Geophys. Res. Lett., 39, L04705. Cohn, T. A., and H. F. Lins, 2005: Nature’s style: Naturally trendy. Geophys. Res. Lett., 32, L23402. Coles, S., 2001: An Introduction to Statistical Modeling of Extreme Values. Springer Science+Business Media, New York, 208 pp. Collaud Coen, M., et al., 2013: Aerosol decadal trends – Part 1: In-situ optical measurements at GAW and IMPROVE stations. Atmos. Chem. Phys., 13, 869–894. Compo, G. P., et al., 2011: The twentieth century reanalysis project. Q. J. Roy. Meteorol. Soc., 137, 1–28. Cooper, O. R., R. S. Gao, D. Tarasick, T. Leblanc, and C. Sweeney, 2012: Long-term ozone trends at rural ozone monitoring sites across the United States, 1990– 2010. J. Geophys. Res., 117, D22307. Cornes, R. C., and P. D. Jones, 2011: An examination of storm activity in the northeast Atlantic region over the 1851–2003 period using the EMULATE gridded MSLP data series. J. Geophys. Res. Atmos., 116, D16110. Coumou, D., A. Robinson, and S. Rahmstorf, 2013: Global increase in record-breaking monthly-mean temperatures. Clim. Change, 118, 771-782. Craigmile, P. F., and P. Guttorp, 2011: Space-time modelling of trends in temperature series. J. Time Ser. Anal., 32, 378–395. Croci-Maspoli, M., C. Schwierz, and H. C. Davies, 2007a: A multifaceted climatology of atmospheric blocking and its recent linear trend. J. Clim., 20, 633–649. Croci-Maspoli, M., C. Schwierz, and H. C. Davies, 2007b: Atmospheric blocking: Space-time links to the NAO and PNA. Clim. Dyn., 29, 713–725. Cutforth, H. W., and D. Judiesch, 2007: Long-term changes to incoming solar energy on the Canadian Prairie. Agr. Forest Meteor., 145, 167–175. Dai, A., 2006: Recent climatology, variability, and trends in global surface humidity. J. Clim., 19, 3589–3606. Dai, A., 2011a: Characteristics and trends in various forms of the Palmer Drought Severity Index during 1900–2008. J. Geophys. Res. Atmos., 116, D12115. Dai, A., 2012: The influence of the inter-decadal Pacific oscillation on US precipitation during 1923–2010. Clim. Dyn., 41, 633-646. Dai, A., 2013: Increasing drought under global warming in observations and models. Nature Clim. Change, 3, 52–58. Dai, A., T. T. Qian, K. E. Trenberth, and J. D. Milliman, 2009: Changes in continental freshwater diSchärge from 1948 to 2004. J. Clim., 22, 2773–2792. Dai, A. G., 2011b: Drought under global warming: A review. Clim. Change, 2, 45–65. Dai, A. G., J. H. Wang, P. W. Thorne, D. E. Parker, L. Haimberger, and X. L. L. Wang, 2011: A new approach to homogenize daily radiosonde humidity data. J. Clim., 24, 965–991. Das, L., J. D. Annan, J. C. Hargreaves, and S. Emori, 2011: Centennial scale warming over Japan: Are the rural stations really rural? Atmos. Sci. Lett., 12, 362-367. Davidson, E., 2009: The contribution of manure and fertilizer nitrogen to atmospheric nitrous oxide since 1860. Nature Geosci., 2, 659–662. Davini, P., C. Cagnazzo, S. Gualdi, and A. Navarra, 2012: Bidimensional diagnostics, variability, and trends of Northern Hemisphere blocking. J. Clim., 25, 6496–6509. Davis, S. M., and K. H. Rosenlof, 2011: A multidiagnostic intercomparison of tropical width time series using reanalyses and satellite observations. J. Clim., 25, 1061-1078. De Laat, A. T. J., and A. N. Maurellis, 2006: Evidence for influence of anthropogenic surface processes on lower tropospheric and surface temperature trends. Int. J. Climatol., 26, 897–913. de Meij, A., A. Pozzer, and J. Lelieveld, 2012: Trend analysis in aerosol optical depths and pollutant emission estimates between 2000 and 2009. Atmos. Environ., 51, 75–85. De Smedt, I., T. Stavrakou, J. F. Müller, R. J. van der A, and M. Van Roozendael, 2010: Trend detection in satellite observations of formaldehyde tropospheric columns. Geophys. Res. Lett., 37, L18808. Dee, D. P., E. Kallen, A. J. Simmons, and L. Haimberger, 2011a: Comments on “Reanalyses suitable for characterizing long-term trends”. Bull. Am. Meteor. Soc., 92, 65–70. Dee, D. P., et al., 2011b: The ERA-Interim reanalysis: Configuration and performance of the data assimilation system. Q. J. R. Meteor. Soc., 137, 553–597. Deeds, D., et al., 2008: Evidence for crustal degassing of CF4 and SF6 in Mojave Desert groundwaters. Geochim. Cosmochim. Acta, 72, 999–1013. DeGaetano, A. T., 2009: Time-dependent changes in extreme-precipitation returnperiod amounts in the continental United States. J. Appl. Meteor. Climatol., 48, 2086–2099. Delgado, J. M., H. Apel, and B. Merz, 2010: Flood trends and variability in the Mekong River. Hydrol. Earth Syst. Sci., 14, 407–418. Della-Marta, P. M., M. R. Haylock, J. Luterbacher, and H. Wanner, 2007a: Doubled length of western European summer heat waves since 1880. J. Geophys. Res. Atmos., 112, D15103. Della-Marta, P. M., J. Luterbacher, H. von Weissenfluh, E. Xoplaki, M. Brunet, and H. Wanner, 2007b: Summer heat waves over western Europe 1880–2003, their relationship to large-scale forcings and predictability. Clim. Dyn., 29, 251–275. Della-Marta, P. M., H. Mathis, C. Frei, M. A. Liniger, J. Kleinn, and C. Appenzeller, 2009: The return period of wind storms over Europe. Int. J. Climatol., 29, 437–459. Deser, C., A. S. Phillips, and M. A. Alexander, 2010a: Twentieth century tropical sea surface temperature trends revisited. Geophys. Res. Lett., 37, L10701. Deser, C., M. A. Alexander, S. P. Xie, and A. S. Phillips, 2010b: Sea surface temperature variability: Patterns and mechanisms. Annu. Rev. Mar. Sci., 2, 115–143. Dessler, A. E., and S. M. Davis, 2010: Trends in tropospheric humidity from reanalysis systems. J. Geophys. Res. Atmos., 115, D19127. Dessler, A. E., Z. Zhang, and P. Yang, 2008: Water-vapor climate feedback inferred from climate fluctuations, 2003–2008. Geophys. Res. Lett., 35, L20704. Diffenbaugh, N. S., J. S. Pal, F. Giorgi, and X. J. Gao, 2007: Heat stress intensification in the Mediterranean climate change hotspot. Geophys. Res. Lett., 34, L11706. Ding, T., W. H. Qian, and Z. W. Yan, 2010: Changes in hot days and heat waves in China during 1961–2007. Int. J. Climatol., 30, 1452–1462. Ding, Y. H., G. Y. Ren, Z. C. Zhao, Y. Xu, Y. Luo, Q. P. Li, and J. Zhang, 2007: Detection, causes and projection of climate change over China: An overview of recent progress. Adv. Atmos. Sci., 24, 954–971. Dlugokencky, E., E. Nisbet, R. Fisher, and D. Lowry, 2011: Global atmospheric methane: Budget, changes and dangers. Philos. Trans. R. Soc. London Ser. A, 369, 2058–2072. Dlugokencky, E., et al., 2005: Conversion of NOAA atmospheric dry air CH4 mole fractions to a gravimetrically prepared standard scale. J. Geophys. Res. Atmos., 110, D18306. Dlugokencky, E., et al., 2009: Observational constraints on recent increases in the atmospheric CH4 burden. Geophys. Res. Lett., L18803. Dlugokencky, E. J., K. A. Masaire, P. M. Lang, P. P. Steele, and E. G. Nisbet, 1994: A dramatic decrease in the growth rate of atmospheric methane in the Northern Hemisphere during 1992. Geophys. Res. Lett., 21, 45–48. Dole, R., et al., 2011: Was there a basis for anticipating the 2010 Russian heat wave? Geophys. Res. Lett., 38, L06702. Donat, M. G., and L. V. Alexander, 2012: The shifting probability distribution of global daytime and night-time temperatures. Geophys. Res. Lett., 39, L14707. Donat, M. G., D. Renggli, S. Wild, L. V. Alexander, G. C. Leckebusch, and U. Ulbrich, 2011: Reanalysis suggests long-term upward trends in European storminess since 1871. Geophys. Res. Lett., 38, L14703. Donat, M. G., L. V. Alexander, H. Yang, I. Durre, R. Vose, and J. Caesar, 2013a: Global land-based datasets for monitoring climatic extremes. Bull. Am. Meteor. Soc., 94, 997-1006. Donat, M. G., et al., 2013b: Changes in extreme temperature and precipitation in the Arab region: Long-term trends and variability related to ENSO and NAO. Int. J. Climatol., doi:10.1002/joc.3707. Donat, M. G., et al., 2013c: Updated analyses of temperature and precipitation extreme indices since the beginning of the twentieth century: The HadEX2 dataset. J. Geophys. Res. Atmos., 118, 2098-2118. Dong, L., T. J. Vogelsang, and S. J. Colucci, 2008: Interdecadal trend and ENSO-related interannual variability in Southern Hemisphere blocking. J. Clim., 21, 3068–3077 Dorigo, W., R. de Jeu, D. Chung, R. Parinussa, Y. Liu, W. Wagner, and D. Fernández-Prieto, 2012: Evaluating global trends (1988–2010) in harmonized multi-satellite surface soil moisture. Geophys. Res. Lett., 39, L18405. Doswell, C., H. Brooks, and N. Dotzek, 2009: On the implementation of the enhanced Fujita scale in the USA. Atmos. Res., 93, 554–563. Douglass, A., et al., 2008: Relationship of loss, mean age of air and the distribution of CFCs to stratospheric circulation and implications for atmospheric lifetimes. J. Geophys. Res. Atmos., 113, D14309. Douglass, A., et al., 2011: WMO/UNEP scientific assessment of ozone depletion: 2010. In: Stratospheric Ozone and Surface Ultraviolet Radiation. World Meteorological Organisation, Geneva, Switzerland. Du, Y., and S. Xie, 2008: Role of atmospheric adjustments in the tropical Indian Ocean warming during the 20th century in climate models. Geophys. Res. Lett., 35, L08712. Du, Y., S. Xie, G. Huang, and K. Hu, 2009: Role of air-sea interaction in the long persistence of El Niño-induced North Indian Ocean warming. J. Clim., 22, 2023–2038. Duan, A. M., and G. X. Wu, 2006: Change of cloud amount and the climate warming on the Tibetan Plateau. Geophys. Res. Lett., 33, L22704. Durre, I., C. N. Williams, X. G. Yin, and R. S. Vose, 2009: Radiosonde-based trends in precipitable water over the Northern Hemisphere: An update. J. Geophys. Res. Atmos., 114, D05112. Dutton, E. G., and B. A. Bodhaine, 2001: Solar irradiance anomalies caused by clearsky transmission variations above Mauna Loa: 1958–99. J. Clim., 14, 3255–3262. Dutton, E. G., D. W. Nelson, R. S. Stone, D. Longenecker, G. Carbaugh, J. M. Harris, and J. Wendell, 2006: Decadal variations in surface solar irradiance as observed in a globally remote network. J. Geophys. Res. Atmos., 111, D19101. Earl, N., S. Dorling, R. Hewston, and R. von Glasow, 2013: 1980–2010 Variability in U.K. surface wind climate. J. Climate, 26, 1172–1191. Easterling, D., and M. Wehner, 2009: Is the climate warming or cooling? Geophys. Res. Lett., 36, L08706. Eastman, R., and S. G. Warren, 2012: A 39-yr survey of cloud changes from land stations worldwide 1971–2009: Long-term trends, relation to aerosols, and expansion of the Tropical Belt. J. Clim., 26, 1286–1303. Eastman, R., S. G. Warren, and C. J. Hahn, 2011: Variations in cloud cover and cloud types over the ocean from surface observations, 1954–2008. J. Clim., 24, 5914– 5934. Ebita, A., et al., 2011: The Japanese 55-year reanalysis “JRA-55”: An interim report. Sola, 7, 149–152. Eccel, E., P. Cau, K. Riemann-Campe, and F. Biasioli, 2012: Quantitative hail monitoring in an alpine area: 35-year climatology and links with atmospheric variables. Int. J. Climatol., 32, 503–517. Efthymiadis, D., C. M. Goodess, and P. D. Jones, 2011: Trends in Mediterranean gridded temperature extremes and large-scale circulation influences. Nat. Hazards Earth Syst. Sci., 11, 2199–2214. Efthymiadis, D. A., and P. D. Jones, 2010: Assessment of maximum possible urbanization influences on land temperature data by comparison of land and marine data around coasts. Atmosphere, 1, 51–61. Elkins, J. W., and G. S. Dutton, 2011: Nitrous oxide and sulfur hexaflouride. Bull. Am. Meteor. Soc., 92, 2. Elsner, J. B., J. P. Kossin, and T. H. Jagger, 2008: The increasing intensity of the strongest tropical cyclones. Nature, 455, 92–95. Emanuel, K., 2007: Environmental factors affecting tropical cyclone power dissipation. J. Clim., 20, 5497–5509. Embury, O., and C. J. Merchant, 2011: Reprocessing for climate of sea surface temperature from the along-track scanning radiometers: A new retrieval scheme. Remote Sens. Environ., 116, 47-61. Embury, O., C. J. Merchant, and G. K. Corlett, 2011: A reprocessing for climate of sea surface temperature from the along-track scanning radiometers: Preliminary validation, accounting for skin and diurnal variability. Remote Sens. Environ., 116, 62-78. Endo, N., and T. Yasunari, 2006: Changes in low cloudiness over China between 1971 and 1996. J. Clim., 19, 1204–1213. Enfield, D. B., A. M. Mestas-Nunez, and P. J. Trimble, 2001: The Atlantic multidecadal oscillation and its relation to rainfall and river flows in the continental US. Geophys. Res. Lett., 28, 2077–2080. Engel, A., et al., 2009: Age of stratospheric air unchanged within uncertainties over the past 30 years. Nature Geosci., 2, 28–31. Espinoza Villar, J. C., et al., 2009: Contrasting regional diSchärge evolutions in the Amazon basin (1974–2004). J. Hydrol., 375, 297–311. Etheridge, D., L. Steele, R. Francey, and R. Langenfelds, 1998: Atmospheric methane between 1000 AD and present: Evidence of anthropogenic emissions and climatic variability. J. Geophys. Res. Atmos., 15979–15993. Etheridge, D. M., L. P. Steele, R. L. Langenfelds, R. J. Francey, J. M. Barnola, and V. I. Morgan, 1996: Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn. J. Geophys. Res. Atmos., 4115–4128. Evan, A. T., A. K. Heidinger, and D. J. Vimont, 2007: Arguments against a physical long-term trend in global ISCCP cloud amounts. Geophys. Res. Lett., 34, L04701. Fall, S., D. Niyogi, A. Gluhovsky, R. A. Pielke, E. Kalnay, and G. Rochon, 2010: Impacts of land use land cover on temperature trends over the continental United States: Assessment using the North American regional reanalysis. Int. J. Climatol., 30, 1980–1993. Fall, S., A. Watts, J. Nielsen-Gammon, E. Jones, D. Niyogi, J. R. Christy, and R. A. Pielke, 2011: Analysis of the impacts of station exposure on the US Historical Climatology Network temperatures and temperature trends. J. Geophys. Res. Atmos., 116, D14120. Falvey, M., and R. D. Garreaud, 2009: Regional cooling in a warming world: Recent temperature trends in the southeast Pacific and along the west coast of subtropical South America (1979–2006). J. Geophys. Res. Atmos., 114, D04102. Favre, A., and A. Gershunov, 2006: Extra-tropical cyclonic/anticyclonic activity in north-eastern Pacific and air temperature extremes in western North America. Clim. Dyn., 26, 617–629. Feng, S., and Q. Hu, 2007: Changes in winter snowfall/precipitation ratio in the contiguous United States. J. Geophys. Res. Atmos., 112, D15109. Ferguson, C. R., and G. Villarini, 2012: Detecting inhomogeneities in the twentieth century reanalysis over the central United States. J. Geophys. Res. Atmos., 117, D05123. Ferranti, L., and P. Viterbo, 2006: The European summer of 2003: Sensitivity to soil water initial conditions. J. Clim., 19, 3659–3680. Ferretti, D., et al., 2005: Unexpected changes to the global methane budget over the past 2000 years. Science, 309, 1714–1717. Fischer, E. M., and C. Schär, 2010: Consistent geographical patterns of changes in high-impact European heatwaves. Nature Geosci., 3, 398–403. Fischer, E. M., S. I. Seneviratne, P. L. Vidale, D. Luthi, and C. Schär, 2007: Soil moisture–atmosphere interactions during the 2003 European summer heat wave. J. Clim., 20, 5081–5099. Fischer, T., M. Gemmer, L. Liu, and B. Su, 2011: Temperature and precipitation trends and dryness/wetness pattern in the Zhujiang River Basin, South China, 1961– 2007. Quatern. Int., 244, 138–148. Fogt, R. L., J. Perlwitz, A. J. Monaghan, D. H. Bromwich, J. M. Jones, and G. J. Marshall, 2009: Historical SAM variability. Part II: Twentieth-century variability and trends from reconstructions, observations, and the IPCC AR4 models. J. Clim., 22, 5346–5365. Folland, C. K., and D. E. Parker, 1995: Correction of instrumental biases in historical sea-surface temperature data. Q. J. R. Meteor. Soc., 121, 319–367. Folland, C. K., D. E. Parker, A. Colman, and W. R., 1999: Large scale modes of ocean surface temperature since the late nineteenth century. In: Beyond El Niño: Decadal and Interdecadal Climate Variability [A. Navarra (ed.)] Springer-Verlag, New York, pp. 73–102. Forster, P., et al., 2007: Changes in atmospheric constituents and in radiative forcing. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor and H. L. Miller (eds.)] Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 129-234. Forster, P. M., et al., 2011: Stratospheric changes and climate. Scientific Assessment of Ozone Depletion: 2010. Global Ozone Research and Monitoring Project– Report No. 52. World Meteorological Organization, Geneva, Switzerland, 1-60. Fortems-Cheiney, A., F. Chevallier, I. Pison, P. Bousquet, S. Szopa, M. N. Deeter, and C. Clerbaux, 2011: Ten years of CO emissions as seen from Measurements of Pollution in the Troposphere (MOPITT). J. Geophys. Res., 116, D05304. Foster, G., and S. Rahmstorf, 2011: Global temperature evolution 1979–2010. Environ. Res. Lett., 6, 044022. Frauenfeld, O. W., and R. E. Davis, 2003: Northern Hemisphere circumpolar vortex trends and climate change implications. J. Geophys. Res. Atmos., 108, 4423. Frederiksen, J. S., and C. S. Frederiksen, 2007: Interdecadal changes in Southern Hemisphere winter storm track modes. Tellus A, 59, 599–617. Free, M., and D. J. Seidel, 2007: Comments on “biases in stratospheric and tropospheric temperature trends derived from historical radiosonde data”. J. Clim., 20, 3704–3709. Free, M., D. J. Seidel, J. K. Angell, J. Lanzante, I. Durre, and T. C. Peterson, 2005: Radiosonde Atmospheric Temperature Products for Assessing Climate (RATPAC): A new data set of large-area anomaly time series. J. Geophys. Res. Atmos., 110, D22101. Frich, P., L. V. Alexander, P. Della-Marta, B. Gleason, M. Haylock, A. Tank, and T. Peterson, 2002: Observed coherent changes in climatic extremes during the second half of the twentieth century. Clim. Res., 19, 193–212. Fu, G. B., S. P. Charles, and J. J. Yu, 2009: A critical overview of pan evaporation trends over the last 50 years. Clim. Change, 97, 193–214. Fu, Q., and P. Lin, 2011: Poleward shift of subtropical jets inferred from satelliteobserved lower stratospheric temperatures. J. Clim., 24, 5597–5603. Fu, Q., C. M. Johanson, S. G. Warren, and D. J. Seidel, 2004: Contribution of stratospheric cooling to satellite-inferred tropospheric temperature trends. Nature, 429, 55–58. Fu, Q., C. M. Johanson, J. M. Wallace, and T. Reichler, 2006: Enhanced mid-latitude tropospheric warming in satellite measurements. Science, 312, 1179–1179. Fueglistaler, S., and P. H. Haynes, 2005: Control of interannual and longer-term variability of stratospheric water vapor. J. Geophys. Res. Atmos., 110, D24108. Fujibe, F., 2009: Detection of urban warming in recent temperature trends in Japan. Int. J. Climatol., 29, 1811–1822. Fujiwara, M., et al., 2010: Seasonal to decadal variations of water vapor in the tropical lower stratosphere observed with balloon-borne cryogenic frost point hygrometers. J. Geophys. Res. Atmos., 115, D18304. Fyfe, J. C., 2003: Extratropical southern hemisphere cyclones: Harbingers of climate change? J. Clim., 16, 2802–2805. Gallant, A., K. Hennessy, and J. Risbey, 2007: Trends in rainfall indices for six Australian regions: 1910–2005. Aust. Meteor. Mag., 56, 223–239. Gallant, A. J. E., and D. J. Karoly, 2010: A Combined Climate Extremes Index for the Australian Region. J. Clim., 23, 6153–6165. Garcia-Herrera, R., J. Diaz, R. M. Trigo, J. Luterbacher, and E. M. Fischer, 2010: A review of the European summer heat wave of 2003. Crit. Rev. Environ. Sci. Technol., 40, 267–306. Gentemann, C., F. Wentz, C. Mears, and D. Smith, 2004: In situ validation of Tropical Rainfall Measuring Mission microwave sea surface temperatures. J. Geophys. Res. Oceans, 109, C04021. Gettelman, A., and Q. Fu, 2008: Observed and simulated upper-tropospheric water vapor feedback. J. Clim., 21, 3282–3289. Gettelman, A., et al., 2010: Multimodel assessment of the upper troposphere and lower stratosphere: Tropics and global trends. J. Geophys. Res. Atmos., 115, D00M08. Gilgen, H., A. Roesch, M. Wild, and A. Ohmura, 2009: Decadal changes in shortwave irradiance at the surface in the period from 1960 to 2000 estimated from Global Energy Balance Archive Data. J. Geophys. Res. Atmos., 114, D00d08. Gillett, N. P., and P. A. Stott, 2009: Attribution of anthropogenic influence on seasonal sea level pressure. Geophys. Res. Lett., 36, L23709. Giorgi, F., and R. Francisco, 2000: Evaluating uncertainties in the prediction of regional climate change. Geophys. Res. Lett., 27, 1295–1298. Giorgi, F., E. S. Im, E. Coppola, N. S. Diffenbaugh, X. J. Gao, L. Mariotti, and Y. Shi, 2011: Higher hydroclimatic intensity with global warming. J. Clim., 24, 5309–5324. Giuntoli, I., B. Renard, J. P. Vidal, and A. Bard, 2013: Low flows in France and their relationship to large-scale climate indices. J. Hydrol., 482, 105-118. Gleason, K. L., J. H. Lawrimore, D. H. Levinson, T. R. Karl, and D. J. Karoly, 2008: A revised US Climate Extremes Index. J. Clim., 21, 2124–2137. Gong, D. Y., and C. H. Ho, 2002: The Siberian High and climate change over middle to high latitude Asia. Theor. Appl. Climatol., 72, 1–9. Gouretski, V., J. Kennedy, T. Boyer, and A. Kohl, 2012: Consistent near-surface ocean warming since 1900 in two largely independent observing networks. Geophys. Res. Lett., 39, L19606. Granier, C., et al., 2011: Evolution of anthropogenic and biomass burning emissions of air pollutants at global and regional scales during the 1980–2010 period. Clim. Change, 109, 163–190. Grant, A. N., S. Brönnimann, and L. Haimberger, 2008: Recent Arctic warming vertical structure contested. Nature, 455, E2–E3. Graversen, R. G., T. Mauritsen, M. Tjernstrom, E. Kallen, and G. Svensson, 2008: Vertical structure of recent Arctic warming. Nature, 451, 53–U54. Greally, B., et al., 2007: Observations of 1,1-difluoroethane (HFC-152a) at AGAGE and SOGE monitoring stations in 1994–2004 and derived global and regional emission estimates. J. Geophys. Res. Atmos., 112, D06308. Griffiths, G. M., et al., 2005: Change in mean temperature as a predictor of extreme temperature change in the Asia-Pacific region. Int. J. Climatol., 25, 1301–1330. Grinsted, A., J. C. Moore, and S. Jevrejeva, 2012: Homogeneous record of Atlantic hurricane surge threat since 1923. Proc. Natl. Acad. Sci. U.S.A. 109, 19601-19605. Groisman, P., R. Knight, and T. Karl, 2012: Changes in intense precipitation over the central United States. J. Hydrometeor., 13, 47–66. Groisman, P., R. Knight, T. R. Karl, D. Easterling, B. M. Sun, and J. Lawrimore, 2004: Contemporary changes of the hydrological cycle over the contiguous United States: Trends derived from in situ observations. J. Hydrometeor., 5, 64–85. Groisman, P. Y., R. W. Knight, D. R. Easterling, T. R. Karl, G. C. Hegerl, and V. A. N. Razuvaev, 2005: Trends in intense precipitation in the climate record. J. Clim., 18, 1326–1350. Gruber, C., and L. Haimberger, 2008: On the homogeneity of radiosonde wind time series. Meteorol. Z., 17, 631–643. Gulev, S. K., O. Zolina, and S. Grigoriev, 2001: Extratropical cyclone variability in the Northern Hemisphere winter from the NCEP/NCAR reanalysis data. Clim. Dyn., 17, 795–809. Guo, H., M. Xu, and Q. Hub, 2010: Changes in near-surface wind speed in China: 1969–2005. Int. J. Climatol., 31, 349-358. Haerter, J., P. Berg, and S. Hagemann, 2010: Heavy rain intensity distributions on varying time scales and at different temperatures. J. Geophys. Res. Atmos., 115, D17102. Haimberger, L., 2007: Homogenization of radiosonde temperature time series using innovation statistics. J. Clim., 20, 1377–1403. Haimberger, L., C. Tavolato, and S. Sperka, 2008: Toward elimination of the warm bias in historic radiosonde temperature records—Some new results from a comprehensive intercomparison of upper-air data. J. Clim., 21, 4587–4606. Haimberger, L., C. Tavolato, and S. Sperka, 2012: Homogenization of the global radiosonde temperature dataset through combined comparison with reanalysis background series and neighboring stations. J. Clim., 25, 8108–8131. Hand, J. L., et al., 2011: IMPROVE, spatial and seasonal patterns and temporal variability of haze and its constituents in the United States. Cooperative Institute for Research in the Atmosphere and Colorado University. Hanna, E., J. Cappelen, R. Allan, T. Jonsson, F. Le Blancq, T. Lillington, and K. Hickey, 2008: New insights into North European and North Atlantic surface pressure variability, storminess, and related climatic change since 1830. J. Clim., 21, 6739–6766. Hannaford, J., and T. Marsh, 2008: High-flow and flood trends in a network of undisturbed catchments in the UK. Int. J. Climatol., 28, 1325–1338. Hansen, J., M. Sato, and R. Ruedy, 2012: Perception of climate change. Proc. Natl. Acad. Sci. U.S.A., 109, E2415–E2423. Hansen, J., R. Ruedy, M. Sato, and K. Lo, 2010: Global surface temperature change. Rev. Geophys., 48, RG4004. Hansen, J., M. Sato, P. Kharecha, and K. von Schuckmann, 2011: Earth’s energy imbalance and implications. Atmos. Chem. Phys., 11, 13421–13449. Harries, J. E., and C. Belotti, 2010: On the variability of the global net radiative energy balance of the nonequilibrium Earth. J. Clim., 23, 1277–1290. Hatzianastassiou, N., C. Matsoukas, A. Fotiadi, K. G. Pavlakis, E. Drakakis, D. Hatzidimitriou, and I. Vardavas, 2005: Global distribution of Earth’s surface shortwave radiation budget. Atmos. Chem. Phys., 5, 2847–2867. Hatzianastassiou, N., C. D. Papadimas, C. Matsoukas, K. Pavlakis, A. Fotiadi, M. Wild, and I. Vardavas, 2012: Recent regional surface solar radiation dimming and brightening patterns: inter-hemispherical asymmetry and a dimming in the Southern Hemisphere. Atmos. Sci. Lett., 13, 43–48. Hausfather, Z., M. J. Menne, C. N. Williams, T. Masters, R. Broberg, and D. Jones, 2013: Quantifying the effect of urbanization on U.S. Historical Climatology Network temperature records. J. Geophys. Res. Atmos., 118, 481-494. Haylock, M. R., et al., 2006: Trends in total and extreme South American rainfall in 1960–2000 and links with sea surface temperature. J. Clim., 19, 1490–1512. He, W. Y., S. P. Ho, H. B. Chen, X. J. Zhou, D. Hunt, and Y. H. Kuo, 2009: Assessment of radiosonde temperature measurements in the upper troposphere and lower stratosphere using COSMIC radio occultation data. Geophys. Res. Lett., 36, L17807. Heidinger, A. K., and M. J. Pavolonis, 2009: Gazing at cirrus clouds for 25 years through a split window. Part I: Methodology. J. Appl. Meteor. Climatol., 48, 1100–1116. Held, I. M., and B. J. Soden, 2006: Robust responses of the hydrological cycle to global warming. J. Clim., 19, 5686–5699. Helmig, D., et al., 2007: A review of surface ozone in the polar regions. Atmos. Environ., 41, 5138–5161. Hidy, G. M., and G. T. Pennell, 2010: Multipollutant air quality management: 2010 critical review. J. Air Waste Manage. Assoc., 60, 645–674. Hilboll, A., A. Richter, and J. P. Burrows, 2013: Long-term changes of tropospheric NO2 over megacities derived from multiple satellite instruments. Atmos. Chem. Phys., 13, 4145-4169. Hinkelman, L. M., P. W. Stackhouse, B. A. Wielicki, T. P. Zhang, and S. R. Wilson, 2009: Surface insolation trends from satellite and ground measurements: Comparisons and challenges. J. Geophys. Res. Atmos., 114, D00d20. Hirdman, D., et al., 2010: Long-term trends of black carbon and sulphate aerosol in the Arctic: Changes in atmospheric transport and source region emissions. Atmos. Chem. Phys., 10, 9351–9368. Hirsch, M. E., A. T. DeGaetano, and S. J. Colucci, 2001: An East Coast winter storm climatology. J. Clim., 14, 882–899. Hirschi, M., et al., 2011: Observational evidence for soil-moisture impact on hot extremes in southeastern Europe. Nature Geosci., 4, 17–21. Ho, S. P., W. He, and Y. H. Kuo, 2009a: Construction of consistent temperature records in the lower stratosphere using Global Positioning System Radio Occultation Data and Microwave Sounding measurements. New Horizons in Occultation Research, Springer-Verlag Berlin, 207–217. Ho, S. P., Y. H. Kuo, Z. Zeng, and T. C. Peterson, 2007: A comparison of lower stratosphere temperature from microwave measurements with CHAMP GPS RO data. Geophys. Res. Lett., 34, L15701. Ho, S. P., M. Goldberg, Y. H. Kuo, C. Z. Zou, and W. Schreiner, 2009b: Calibration of temperature in the lower stratosphere from microwave measurements using COSMIC radio occultation data: Preliminary results. Terr. Atmos. Ocean. Sci., 20, 87–100. Ho, S. P., et al., 2012: Reproducibility of GPS radio occultation data for climate monitoring: Profile-to-profile inter-comparison of CHAMP climate records 2002 to 2008 from six data centers. J. Geophys. Res. Atmos., 117, D18111. Hoerling, M., et al., 2012: Anatomy of an extreme event. J. Clim., 26, 2811–2832. Holben, B. N., et al., 1998: AERONET—A federated instrument network and data archive for aerosol characterization. Remote Sens. Environ., 66, 1–16. Holland, G. J., and P. J. Webster, 2007: Heightened tropical cyclone activity in the North Atlantic: Natural variability or climate trend? Philos. Trans. R. Soc. London Ser. A, 365, 2695–2716. Hope, P. K., W. Drosdowsky, and N. Nicholls, 2006: Shifts in the synoptic systems influencing southwest Western Australia. Clim. Dyn., 26, 751–764. Hsu, N. C., et al., 2012: Global and regional trends of aerosol optical depth over land and ocean using SeaWiFS measurements from 1997 to 2010. Atmos. Chem. Phys. Discuss., 12, 8465–8501. Hsu, P. C., T. Li, and B. Wang, 2011: Trends in global monsoon area and precipitation over the past 30 years. Geophys. Res. Lett., 38, L08701. Hu, Y., and Q. Fu, 2007: Observed poleward expansion of the Hadley circulation since 1979. Atmos. Chem. Phys., 7, 5229–5236. Hu, Y. C., W. J. Dong, and Y. He, 2010: Impact of land surface forcings on mean and extreme temperature in eastern China. J. Geophys. Res. Atmos., 115, 11. Hu, Y. Y., C. Zhou, and J. P. Liu, 2011: Observational evidence for the poleward expansion of the Hadley circulation. Adv. Atmos. Sci., 28, 33–44. Huang, J., et al., 2008: Estimation of regional emissions of nitrous oxide from 1997 to 2005 using multinetwork measurements, a chemical transport model, and an inverse method. J. Geophys. Res. Atmos., 113, D17313. Huang, W.-R., S.-Y. Wang, and J. C. L. Chan, 2010: Discrepancies between global reanalyses and observations in the interdecadal variations of Southeast Asian cold surge. Int. J. Climatol., 31, 2272-2280.. Hudson, R. D., 2012: Measurements of the movement of the jet streams at mid-latitudes, in the Northern and Southern Hemispheres, 1979 to 2010. Atmos. Chem. Phys., 12, 7797–7808. Hudson, R. D., M. F. Andrade, M. B. Follette, and A. D. Frolov, 2006: The total ozone field separated into meteorological regimes—Part II: Northern Hemisphere midlatitude total ozone trends. Atmos. Chem. Phys., 6, 5183–5191. Hundecha, Y., A. St-Hilaire, T. Ouarda, S. El Adlouni, and P. Gachon, 2008: A nonstationary extreme value analysis for the assessment of changes in extreme annual wind speed over the Gulf of St. Lawrence, Canada. J. Appl. Meteor. Climatol., 47, 2745–2759. Hurrell, J. W., 1995: Decadal trends in the North Atlantic Oscillation: Regional temperatures and precipitation. Science, 269, 676–679. Hurst, D., 2011: Stratospheric water vapor trends over Boulder, Colorado: Analysis of the 30 year Boulder record. J. Geophys. Res., 116, D02306. Idso, S. B., and A. J. Brazel, 1984: Rising atmospheric carbon-dioxide concentrations may increase streamflow. Nature, 312, 51–53. IPCC, 2007: Clim. Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor and H. L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 996 pp. Ishii, M., A. Shouji, S. Sugimoto, and T. Matsumoto, 2005: Objective analyses of seasurface temperature and marine meteorological variables for the 20th century using icoads and the Kobe collection. Int. J. Climatol., 25, 865–879. Ishijima, K., et al., 2007: Temporal variations of the atmospheric nitrous oxide concentration and its delta N-15 and delta O-18 for the latter half of the 20th century reconstructed from firn air analyses. J. Geophys. Res. Atmos., 112, D03305 . Jain, S. K., and V. Kumar, 2012: Trend analysis of rainfall and temperature data for India. Curr. Sci., 102, 37–49. Jakob, D., D. Karoly, and A. Seed, 2011: Non-stationarity in daily and sub-daily intense rainfall—Part 2: Regional assessment for sites in south-east Australia. Nat. Hazards Earth Syst. Sci., 11, 2273–2284. Jhajharia, D., S. Shrivastava, D. Sarkar, and S. Sarkar, 2009: Temporal characteristics of pan evaporation trends under humid conditions of northeast India. Agr. Forest Meteorol., 336, 61–73. Jiang, T., Z. W. Kundzewicz, and B. Su, 2008: Changes in monthly precipitation and flood hazard in the Yangtze River Basin, China. Int. J. Climatol., 28, 1471–1481. Jiang, X., W. Ku, R. Shia, Q. Li, J. Elkins, R. Prinn, and Y. Yung, 2007: Seasonal cycle of N2O: Analysis of data. Global Biogeochem. Cycles, 21, GB1006. Jiang, Y., Y. Luo, Z. C. Zhao, and S. W. Tao, 2010: Changes in wind speed over China during 1956–2004. Theor. Appl. Climatol., 99, 421–430. Jin, S. G., J. U. Park, J. H. Cho, and P. H. Park, 2007: Seasonal variability of GPS-derived zenith tropospheric delay (1994–2006) and climate implications. J. Geophys. Res. Atmos., 112, D09110. John, V. O., R. P. Allan, and B. J. Soden, 2009: How robust are observed and simulated precipitation responses to tropical ocean warming? Geophys. Res. Lett., 36, L14702. John, V. O., G. Holl, R. P. Allan, S. A. Buehler, D. E. Parker, and B. J. Soden, 2011: Clearsky biases in satellite infrared estimates of upper tropospheric humidity and its trends. J. Geophys. Res. Atmos., 116, D14108. Jones, D. A., W. Wang, and R. Fawcett, 2009: High-quality spatial climate data-sets for Australia. Australian, Meteor. Ocean. J., 58, 233–248. Jones, P. D., and D. H. Lister, 2007: Intercomparison of four different Southern Hemisphere sea level pressure datasets. Geophys. Res. Lett., 34, L10704. Jones, P. D., and D. H. Lister, 2009: The urban heat island in Central London and urban-related warming trends in Central London since 1900. Weather, 64, 323–327. Jones, P. D., T. Jonsson, and D. Wheeler, 1997: Extension to the North Atlantic Oscillation using early instrumental pressure observations from Gibraltar and southwest Iceland. Int. J. Climatol., 17, 1433–1450. Jones, P. D., D. H. Lister, and Q. Li, 2008: Urbanization effects in large-scale temperature records, with an emphasis on China. J. Geophys. Res. Atmos., 113, D16122. Jones, P. D., D. H. Lister, T. J. Osborn, C. Harpham, M. Salmon, and C. P. Morice, 2012: Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010. J. Geophys. Res. Atmos., 117, D05127. Jones, R., S. Westra, and A. Sharma, 2010: Observed relationships between extreme sub-daily precipitation, surface temperature, and relative humidity. Geophys. Res. Lett., 37, L22805. Joshi, M. M., J. M. Gregory, M. J. Webb, D. M. H. Sexton, and T. C. Johns, 2008: Mechanisms for the land/sea warming contrast exhibited by simulations of climate change. Clim. Dyn., 30, 455–465. Jovanovic, B., D. Collins, K. Braganza, D. Jakob, and D. A. Jones, 2011: A high-quality monthly total cloud amount dataset for Australia. Clim. Change, 108, 485-517. Jung, M., et al., 2010: Recent decline in the global land evapotranspiration trend due to limited moisture supply. Nature, 467, 951–954. Kahn, R. A., et al., 2007: Satellite-derived aerosol optical depth over dark water from MISR and MODIS: Comparisons with AERONET and implications for climatological studies. J. Geophys. Res. Atmos., 112, D18205 Kanamitsu, M., W. Ebisuzaki, J. Woollen, S. K. Yang, J. J. Hnilo, M. Fiorino, and G. L. Potter, 2002: NCEP-DOE AMIP-II reanalysis (R-2). Bull. Am. Meteor. Soc., 83, 1631–1643. Kang, S. M., L. M. Polvani, J. C. Fyfe, and M. Sigmond, 2011: Impact of polar ozone depletion on subtropical Precipitation. Science, 332, 951–954. Kao, H. Y., and J. Y. Yu, 2009: Contrasting Eastern-Pacific and Central-Pacific types of ENSO. J. Clim., 22, 615–632. Karnauskas, K. B., R. Seager, A. Kaplan, Y. Kushnir, and M. A. Cane, 2009: Observed strengthening of the zonal sea surface temperature gradient across the equatorial Pacific Ocean. J. Clim., 22, 4316–4321. Karnieli, A., et al., 2009: Temporal trend in anthropogenic sulfur aerosol transport from central and eastern Europe to Israel. J. Geophys. Res. Atmos., 114, D00d19. Karoly, D., 1989: Southern-Hemisphere circulation features associated with El NiñoSouthern Oscillation. J. Clim., 2, 1239–1252. Kato, S., et al.: Surface irradiances consistent with CERES-derived top-of-atmosphere shortwave and longwave irradiances. J. Clim. 26, 2719-2740 Keeling, C., R. Bacastow, A. Bainbridge, C. Ekdahl, P. Guenther, L. Waterman, and J. Chin, 1976a: Atmospheric Carbon-Dioxide Variations at Mauna-Loa Observatory, Hawaii. Tellus, 28, 538–551. Keeling, C. D., J. A. Adams, and C. A. Ekdahl, 1976b: Atmospheric carbo-dioxide variations at South Pole. Tellus, 28, 553–564. Keller, C., D. Brunner, S. Henne, M. Vollmer, S. O’Doherty, and S. Reimann, 2011: Evidence for under-reported western European emissions of the potent greenhouse gas HFC-23. Geophys. Res. Lett., 38, L15808. Kennedy, J. J., N. A. Rayner, and R. O. Smith, 2012: Using AATSR data to assess the quality of in situ sea surface temperature observations for climate studies. Remote Sens. Environ., 116, 79–92. Kennedy, J. J., N. A. Rayner, R. O. Smith, D. E. Parker, and M. Saunby, 2011a: Reassessing biases and other uncertainties in sea surface temperature observations measured in situ since 1850: 2. Biases and homogenization. J. Geophys. Res. Atmos., 116, D14104. Kennedy, J. J., N. A. Rayner, R. O. Smith, M. Saunby, and D. E. Parker, 2011b: Reassessing biases and other uncertainties in sea surface temperature observations since 1850, part 1: Measurement and sampling uncertainties. J. Geophys. Res., 116, D14103. Kent, E. C., and D. I. Berry, 2008: Assessment of the Marine Observing System (ASMOS): Final report. National Oceanography Centre Southampton Research and Consultancy Report, 55 pp. Kent, E. C., S. D. Woodruff, and D. I. Berry, 2007: Metadata from WMO publication no. 47 and an assessment of voluntary observing ship observation heights in ICOADS. J. Atmos. Ocean Technol., 24, 214–234. Kent, E. C., S. Fangohr, and D. I. Berry, 2012: A comparative assessment of monthly mean wind speed products over the global ocean. Int. J. Climatol., 33, 2530- 2541. Kent, E. C., J. J. Kennedy, D. I. Berry, and R. O. Smith, 2010: Effects of instrumentation changes on sea surface temperature measured in situ. Clim. Change, 1, 718–728. Kent, E. C., N. A. Rayner, D. I. Berry, M. Saunby, B. I. Moat, J. J. Kennedy, and D. E. Parker, 2013: Global analysis of night marine air temperature and its uncertainty since 1880, the HadNMAT2 Dataset, J. Geophys. Res., 118, 1281-1298. Kenyon, J., and G. C. Hegerl, 2008: Influence of modes of climate variability on global temperature extremes. J. Clim., 21, 3872–3889. Kenyon, J., and G. C. Hegerl, 2010: Influence of modes of climate variability on global precipitation extremes. J. Clim., 23, 6248–6262. Kharin, V., F. Zwiers, X. Zhang, and M. Wehner, 2013: Changes in temperature and precipitation extremes in the CMIP5 ensemble. Climatic Change, 119, 345-357. Kiehl, J. T., and K. E. Trenberth, 1997: Earth’s annual global mean energy budget. Bull. Am. Meteor. Soc., 78, 197–208. Kim, D., and V. Ramanathan, 2012: Improved estimates and understanding of global albedo and atmospheric solar absorption. Geophys. Res. Lett., 39, L24704. Kim, D. Y., and V. Ramanathan, 2008: Solar radiation budget and radiative forcing due to aerosols and clouds. J. Geophys. Res. Atmos., 113, D02203. Kim, J., et al., 2010: Regional atmospheric emissions determined from measurements at Jeju Island, Korea: Halogenated compounds from China. Geophys. Res. Lett., 37, L12801. King, A., L. Alexander, and M. Donat, 2013: The efficacy of using gridded data to examine extreme rainfall characteristics: A case study for Australia. Inter. J. Climatol., 33, 2376-2387. Kistler, R., et al., 2001: The NCEP-NCAR 50-year reanalysis: Monthly means CD-ROM and documentation. Bull. Am. Meteor. Soc., 82, 247–267. Klein Tank, A. M. G., et al., 2006: Changes in daily temperature and precipitation extremes in central and south Asia. J. Geophys. Res. Atmos., 111, D16105. Klok, E. J., and A. Tank, 2009: Updated and extended European dataset of daily climate observations. Int. J. Climatol., 29, 1182–1191. Knapp, K. R., and M. C. Kruk, 2010: Quantifying interagency differences in tropical cyclone best-track wind speed estimates. Mon. Weather Rev., 138, 1459–1473. Knowles, N., M. D. Dettinger, and D. R. Cayan, 2006: Trends in snowfall versus rainfall in the western United States. J. Clim., 19, 4545–4559. Knutson, T. R., et al., 2010: Tropical cyclones and climate change. Nature Geosci., 3, 157–163. Kobayashi, S., M. Matricardi, D. Dee, and S. Uppala, 2009: Toward a consistent reanalysis of the upper stratosphere based on radiance measurements from SSU and AMSU-A. Q. J. R. Meteorol. Soc., 135, 2086–2099. Kopp, G., and G. Lawrence, 2005: The Total Irradiance Monitor (TIM): Instrument design. Solar Phys., 230, 91–109. Kopp, G., and J. L. Lean, 2011: A new, lower value of total solar irradiance: Evidence and climate significance. Geophys. Res. Lett., 38, L01706. Kopp, G., G. Lawrence, and G. Rottman, 2005: The Total Irradiance Monitor (TIM): Science results. Solar Phys., 230, 129–139. Kossin, J. P., K. R. Knapp, D. J. Vimont, R. J. Murnane, and B. A. Harper, 2007: A globally consistent reanalysis of hurricane variability and trends. Geophys. Res. Lett., 34, L04815. Koutsoyiannis, D., and A. Montanari, 2007: Statistical analysis of hydroclimatic time series: Uncertainty and insights. Water Resour. Res., 43, W05429. Kreienkamp, F., A. Spekat, and W. Enke, 2010: Stationarity of atmospheric waves and blocking over Europe-based on a reanalysis dataset and two climate scenarios. Theor. Appl. Climatol., 102, 205–212. Krishna Moorthy, K., S. Suresh Babu, and S. K. Satheesh, 2007: Temporal heterogeneity in aerosol characteristics and the resulting radiative impact at a tropical coastal station—Part 1: Microphysical and optical properties. Ann. Geophys., 25, 2293–2308. Krishna Moorthy, K., S. Suresh Babu, M. R. Manoj, and S. K. Satheesh, 2013: Buildup of Aerosols over the Indian Region. Geophys. Res. Lett., 40, 1011-1014 Krishna Moorthy, K., S. S. Babu, S. K. Satheesh, S. Lal, M. M. Sarin, and S. Ramachandran, 2009: Climate implications of atmospheric aerosols and trace gases: Indian Scenario, Climate Sense. World Meteorological Organisation, Geneva, Switzerland, pp. 157–160. Krueger, O., F. Schenk, F. Feser, and R. Weisse, 2013: Inconsistencies between longterm trends in storminess derived from the 20CR reanalysis and observations. J. Clim., 26, 868–874. Kruger, A., and S. Sekele, 2013: Trends in extreme temperature indices in South Africa: 1962–2009. Int. J. Climatol., 33, 661-676. Kubota, H., and J. C. L. Chan, 2009: Interdecadal variability of tropical cyclone landfall in the Philippines from 1902 to 2005. Geophys. Res. Lett., 36, L12802. Kudo, R., A. Uchiyama, A. Yamazaki, T. Sakami, and O. Ijima, 2011: Decadal changes in aerosol optical thickness and single scattering albedo estimated from groundbased broadband radiometers: A case study in Japan. J. Geophys. Res., 116, D03207. Kudo, R., A. Uchiyama, O. Ijima, N. Ohkawara, and S. Ohta, 2012: Aerosol impact on the brightening in Japan. J. Geophys. Res. Atmos., 117, 11. Kueppers, L. M., M. A. Snyder, and L. C. Sloan, 2007: Irrigation cooling effect: Regional climate forcing by land-use change. Geophys. Res. Lett., 34, L03703. Kuglitsch, F. G., A. Toreti, E. Xoplaki, P. M. Della-Marta, J. Luterbacher, and H. Wanner, 2009: Homogenization of daily maximum temperature series in the Mediterranean. J. Geophys. Res. Atmos., 114, D15108. Kuglitsch, F. G., A. Toreti, E. Xoplaki, P. M. Della-Marta, C. S. Zerefos, M. Turkes, and J. Luterbacher, 2010: Heat wave changes in the eastern Mediterranean since 1960. Geophys. Res. Lett., 37, L04802. Kumari, B. P., and B. N. Goswami, 2010: Seminal role of clouds on solar dimming over the Indian monsoon region. Geophys. Res. Lett., 37, L06703. Kumari, B. P., A. L. Londhe, S. Daniel, and D. B. Jadhav, 2007: Observational evidence of solar dimming: Offsetting surface warming over India. Geophys. Res. Lett., 34, L21810. Kundzewicz, Z. W., et al., 2007: Freshwater resources and their management. Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor and H. L. Miller (eds.)].Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA,172-210. Kunkel, K. E., M. A. Palecki, L. Ensor, D. Easterling, K. G. Hubbard, D. Robinson, and K. Redmond, 2009: Trends in twentieth-century US extreme snowfall seasons. J. Clim., 22, 6204–6216. Kunkel, K. E., et al., 2008: Observed changes in weather and climate extremes. In: Weather and Climate Extremes in a Changing Climate. Regions of Focus: North America, Hawaii, Caribbean, and U.S. Pacific Islands [T. R. Karl, G. A. Meehl, D. M. Christopher, S. J. Hassol, A. M. Waple, and W. L. Murray (eds.)]. A Report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research. Kunz, M., J. Sander, and C. Kottmeier, 2009: Recent trends of thunderstorm and hailstorm frequency and their relation to atmospheric characteristics in southwest Germany. Int. J. Climatol., 29, 2283–2297. Kuo, Y. H., W. S. Schreiner, J. Wang, D. L. Rossiter, and Y. Zhang, 2005: Comparison of GPS radio occultation soundings with radiosondes. Geophys. Res. Lett., 32, L05817. Kvalevag, M. M., and G. Myhre, 2007: Human impact on direct and diffuse solar radiation during the industrial era. J. Clim., 20, 4874–4883. L’Ecuyer, T. S., N. B. Wood, T. Haladay, G. L. Stephens, and P. W. Stackhouse, 2008: Impact of clouds on atmospheric heating based on the R04 CloudSat fluxes and heating rates data set. J. Geophys. Res. Atmos., 113, 15. Labat, D., Y. Godderis, J. L. Probst, and J. L. Guyot, 2004: Evidence for global runoff increase related to climate warming. Adv. Water Resour., 27, 631–642. Ladstadter, F., A. K. Steiner, U. Foelsche, L. Haimberger, C. Tavolato, and G. Kirchnebngast, 2011: An assessment of differences in lower stratospheric temperature records from (A)MSU, radiosondes and GPS radio occultation. Atmos. Meas. Tech., 4, 1965–1977. Landsea, C. W., 2007: Counting Atlantic tropical cyclones back to 1900. EOS Trans. (AGU), 88, 197–202. Landsea, C. W., B. A. Harper, K. Hoarau, and J. A. Knaff, 2006: Can we detect trends in extreme tropical cyclones? Science, 313, 452–454. Landsea, C. W., et al., 2011: A reanalysis of the 1921–30 Atlantic Hurricane Database. J. Clim., 25, 865–885. Langematz, U., and M. Kunze, 2008: Dynamical changes in the Arctic and Antarctic stratosphere during spring. In: Climate Variability and Extremes during the Past 100 Years. Advances in Global Change Research [S. Brönnimann, J. Luterbacher, T. Ewen, H. F. Diaz, R. S. Stolarski, and U. Neu (eds.)], Springer, pp. 293–301. Lanzante, J. R., 2009: Comment on “Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection” by Karen H. Rosenlof and George C. Reid. J. Geophys. Res. Atmos., 114, D12104. Laprise, R., 1992: The resolution of global spectroal models. Bull. Am. Meteor. Soc., 73, 1453–1454. Larkin, N. K., and D. E. Harrison, 2005: On the definition of El Niño and associated seasonal average US weather anomalies. Geophys. Res. Lett., 32, L13705. Lawrimore, J. H., M. J. Menne, B. E. Gleason, C. N. Williams, D. B. Wuertz, R. S. Vose, and J. Rennie, 2011: An overview of the Global Historical Climatology Network monthly mean temperature data set, version 3. J. Geophys. Res. Atmos., 116, D19121. Leakey, A. D. B., M. Uribelarrea, E. A. Ainsworth, S. L. Naidu, A. Rogers, D. R. Ort, and S. P. Long, 2006: Photosynthesis, productivity, and yield of maize are not affected by open-air elevation of CO2 concentration in the absence of drought. Plant Physiol., 140, 779–790. Lee, H. T., A. Gruber, R. G. Ellingson, and I. Laszlo, 2007: Development of the HIRS outgoing longwave radiation climate dataset. J. Atmos. Ocean Technol., 24, 2029–2047. Lefohn, A. S., D. Shadwick, and S. J. Oltmans, 2010: Characterizing changes in surface ozone levels in metropolitan and rural areas in the United States for 1980–2008 and 1994–2008. Atmos. Environ., 44, 5199–5210. Lehmann, A., K. Getzlaff, and J. Harlass, 2011: Detailed assessment of climate variability in the Baltic Sea area for the period 1958 to 2009. Clim. Res., 46, 185– 196. Lelieveld, J., J. van Aardenne, H. Fischer, M. de Reus, J. Williams, and P. Winkler, 2004: Increasing ozone over the Atlantic Ocean. Science, 304, 1483–1487. Lenderink, G., and E. Van Meijgaard, 2008: Increase in hourly precipitation extremes beyond expectations from temperature changes. Nature Geosci., 1, 511–514. Lenderink, G., H. Y. Mok, T. C. Lee, and G. J. van Oldenborgh, 2011: Scaling and trends of hourly precipitation extremes in two different climate zones – Hong Kong and the Netherlands. Hydrol. Earth Syst. Sci. Discuss., 8, 4701–4719. Lennartz, S., and A. Bunde, 2009: Trend evaluation in records with long-term memory: Application to global warming. Geophys. Res. Lett., 36, L16706. Levin, I., et al., 2010: The global SF6 source inferred from long-term high precision atmospheric measurements and its comparison with emission inventories. Atmos. Chem. Phys., 10, 2655–2662. End Part 1
 
Begin Part 2
Levitus, S., J. I. Antonov, T. P. Boyer, R. A. Locarnini, H. E. Garcia, and A. V. Mishonov, 2009: Global ocean heat content 1955–2008 in light of recently revealed instrumentation problems. Geophys. Res. Lett., 36, 5. Levy, R. C., L. A. Remer, R. G. Kleidman, S. Mattoo, C. Ichoku, R. Kahn, and T. F. Eck, 2010: Global evaluation of the Collection 5 MODIS dark-target aerosol products over land. Atmos. Chem. Phys., 10, 10399–10420. Li, Q., H. Zhang, X. Liu, J. Chen, W. Li, and P. Jones, 2009: A mainland China homogenized historical temperature dataset of 1951–2004. Bull. Am. Meteor. Soc., 90, 1062–1065. Li, Q., W. Dong, W. Li, X. Gao, P. Jones, J. Kennedy, and D. Parker, 2010a: Assessment of the uncertainties in temperature change in China during the last century. Chin. Sci. Bull., 55, 1974–1982. Li, Q. X., et al., 2010b: Assessment of surface air warming in northeast China, with emphasis on the impacts of urbanization. Theor. Appl. Climatol., 99, 469–478. Li, Z., et al., 2012: Changes of daily climate extremes in southwestern China during 1961–2008. Global Planet. Change, 80–81, 255–272. Liang, F., and X. A. Xia, 2005: Long-term trends in solar radiation and the associated climatic factors over China for 1961–2000. Ann. Geophys., 23, 2425–2432. Liebmann, B., R. M. Dole, C. Jones, I. Blade, and D. Allured, 2010: Influence of choice of time period on global surface temperature trend estimates. Bull. Am. Meteor. Soc., 91, 1485–U1471. Liepert, B. G., 2002: Observed reductions of surface solar radiation at sites in the United States and worldwide from 1961 to 1990. Geophys. Res. Lett., 29, 1421. Liley, J. B., 2009: New Zealand dimming and brightening. J. Geophys. Res. Atmos., 114, D00d10. Lim, E. P., and I. Simmonds, 2007: Southern Hemisphere winter extratropical cyclone characteristics and vertical organization observed with the ERA-40 data in 1979–2001. J. Clim., 20, 2675–2690. Lim, E. P., and I. Simmonds, 2009: Effect of tropospheric temperature change on the zonal mean circulation and SH winter extratropical cyclones. Clim. Dyn., 33, 19–32. Lim, Y. K., M. Cai, E. Kalnay, and L. Zhou, 2008: Impact of vegetation types on surface temperature change. J. Appl. Meteor. Climatol., 47, 411–424. Lin, C., K. Yang, J. Qin, and R. Fu, 2012: Observed coherent trends of surface and upper-air wind speed over China since 1960. J. Clim.,26, 2891-2903.. Liu, B., M. Xu, and M. Henderson, 2011: Where have all the showers gone? Regional declines in light precipitation events in China, 1960–2000. Int. J. Climatol., 31, 1177–1191. Liu, B. H., M. Xu, M. Henderson, and W. G. Gong, 2004a: A spatial analysis of pan evaporation trends in China, 1955–2000. J. Geophys. Res. Atmos., 109, D15102. Liu, B. H., M. Xu, M. Henderson, Y. Qi, and Y. Q. Li, 2004b: Taking China’s temperature: Daily range, warming trends, and regional variations, 1955–2000. J. Clim., 17, 4453–4462. Liu, Q. H., and F. Z. Weng, 2009: Recent stratospheric temperature observed from satellite measurements. Sola, 5, 53–56. Lo, M.-H., and J. S. Famiglietti, 2013: Irrigation in California’s Central Valley strengthens the southwestern U.S. water cycle. Geophys. Res. Lett., 40, 301-306. Loeb, N. G., et al., 2009: Toward optimal closure of the Earth’s top-of-atmosphere radiation budget. J. Clim., 22, 748–766. Loeb, N. G., et al., 2012a: Advances in understanding top-of-atmosphere radiation variability from satellite observations. Surv. Geophys., 33, 359–385. Loeb, N. G., et al., 2012b: Observed changes in top-of-the-atmosphere radiation and upper-ocean heating consistent within uncertainty. Nature Geosci., 5, 110–113. Logan, J. A., et al., 2012: Changes in ozone over Europe since 1990: Analysis of ozone measurements from sondes, regular aircraft (MOZAIC), and alpine surface sites. J. Geophys. Res., 117, D09301. Long, C. N., E. G. Dutton, J. A. Augustine, W. Wiscombe, M. Wild, S. A. McFarlane, and C. J. Flynn, 2009: Significant decadal brightening of downwelling shortwave in the continental United States. J. Geophys. Res. Atmos., 114, D00d06 Lorenz, R., E. B. Jaeger, and S. I. Seneviratne, 2010: Persistence of heat waves and its link to soil moisture memory. Geophys. Res. Lett., 37, L09703. Lucas, C., H. Nguyen, and B. Timbal, 2012: An observational analysis of Southern Hemisphere tropical expansion. J. Geohys. Res., 117, D17112. Luo, J. J., W. Sasaki, and Y. Masumoto, 2012: Indian Ocean warming modulates Pacific climate change. Proc. Natl. Acad. Sci. U.S.A., 109, 18701–18706. Lupikasza, E., 2010: Spatial and temporal variability of extreme precipitation in Poland in the period 1951–2006. Int. J. Climatol., 30, 991–1007. Lyman, J. M., et al., 2010: Robust warming of the global upper ocean. Nature, 465, 334–337. Lynch, A. H., J. A. Curry, R. D. Brunner, and J. A. Maslanik, 2004: Toward an integrated assessment of the impacts of extreme wind events on Barrow, Alaska. Bull. Am. Meteor. Soc., 85, 209–. Mahowald, N., et al., 2010: Observed 20th century desert dust variability: Impact on climate and biogeochemistry. Atmos. Chem. Phys., 10, 10875–10893. Makowski, K., M. Wild, and A. Ohmura, 2008: Diurnal temperature range over Europe between 1950 and 2005. Atmos. Chem. Phys., 8, 6483–6498. Makowski, K., E. B. Jaeger, M. Chiacchio, M. Wild, T. Ewen, and A. Ohmura, 2009: On the relationship between diurnal temperature range and surface solar radiation in Europe. J. Geophys. Res. Atmos., 114, D00d07. Manabe, S., and R. F. Strickler, 1964: Thermal equilibrium of the atmosphere with a convective adjustment. Journal of the Atmospheric Sciences, 21, 361–385. Mann, M. E., 2011: On long range dependence in global surface temperature series. Clim. Change, 107, 267–276. Mann, M. E., T. A. Sabbatelli, and U. Neu, 2007a: Evidence for a modest undercount bias in early historical Atlantic tropical cyclone counts. Geophys. Res. Lett., 34, L22707. Mann, M. E., K. A. Emanual, G. J. Holland, and P. J. Webster, 2007b: Atlantic tropical cyclones revisited. EOS Transactions (AGU), 88, 349–350. Manney, G. L., et al., 2011: Unprecedented Arctic ozone loss in 2011. Nature, 478, 469–475. Mantua, N. J., S. R. Hare, Y. Zhang, J. M. Wallace, and R. C. Francis, 1997: A Pacific interdecadal climate oscillation with impacts on salmon production. Bull. Am. Meteor. Soc., 78, 1069–1079. Marenco, A., H. Gouget, P. Nédélec, and J. P. Pagés, 1994: Evidence of a long-term increase in tropospheric ozone from Pic du Midi series: Consequences: positive radiative forcing. J. Geophys. Res., 99, 16,617–616, 632. Marshall, G. J., 2003: Trends in the southern annular mode from observations and reanalyses. J. Clim., 16, 4134–4143. Martinerie, P., et al., 2009: Long-lived halocarbon trends and budgets from atmospheric chemistry modelling constrained with measurements in polar firn. Atmos. Chem. Phys., 3911–3934. Mastrandrea, M., et al., 2011: The IPCC AR5 guidance note on consistent treatment of uncertainties: A common approach across the working groups. Clim. Change, 108, 675–691. Matulla, C., W. Schoner, H. Alexandersson, H. von Storch, and X. L. Wang, 2008: European storminess: Late nineteenth century to present. Clim. Dyn., 31, 125–130. McCarthy, M. P., P. W. Thorne, and H. A. Titchner, 2009: An analysis of tropospheric humidity trends from radiosondes. J. Clim., 22, 5820–5838. McCarthy, M. P., H. A. Titchner, P. W. Thorne, S. F. B. Tett, L. Haimberger, and D. E. Parker, 2008: Assessing bias and uncertainty in the HadAT-adjusted radiosonde climate record. J. Clim., 21, 817–832. McKitrick, R., 2010: Atmospheric circulations do not explain the temperature-industrialization correlation. Stat. Politics Policy, 1, issue 1 . McKitrick, R., and P. J. Michaels, 2004: A test of corrections for extraneous signals in gridded surface temperature data. Clim. Res., 26, 159–173. McKitrick, R., and N. Nierenberg, 2010: Socioeconomic patterns in climate data. J. Econ. Soc. Meas, 35, 149–175. McKitrick, R. R., and P. J. Michaels, 2007: Quantifying the influence of anthropogenic surface processes and inhomogeneities on gridded global climate data. J. Geophys. Res. Atmos., 112, D24S09. McNider, R. T., et al., 2012: Response and sensitivity of the nocturnal boundary layer over land to added longwave radiative forcing. J. Geophys. Res., 117, D14106. McVicar, T. R., T. G. Van Niel, L. T. Li, M. L. Roderick, D. P. Rayner, L. Ricciardulli, and R. J. Donohue, 2008: Wind speed climatology and trends for Australia, 1975–2006: Capturing the stilling phenomenon and comparison with near-surface reanalysis output. Geophys. Res. Lett., 35, L20403. McVicar, T. R., et al., 2012: Global review and synthesis of trends in observed terrestrial near-surface wind speeds: Implications for evaporation. J. Hydrol., 416, 182–205. Mears, C., J. Wang, S. Ho, L. Zhang, and X. Zhou, 2010: Total column water vapor, in State of the Climate in 2009. Bull. Am. Meteor. Soc. [D. S. Arndt, M. O. Baringer, and M. R. Johnson (eds.)]. Mears, C. A., and F. J. Wentz, 2009a: Construction of the remote sensing systems V3.2 atmospheric temperature records from the MSU and AMSU microwave sounders. J. Atmos. Ocean Technol., 26, 1040–1056. Mears, C. A., and F. J. Wentz, 2009b: Construction of the RSS V3.2 lower-tropospheric temperature dataset from the MSU and AMSU microwave sounders. J. Atmos. Ocean Technol., 26, 1493–1509. Mears, C. A., F. J. Wentz, and P. W. Thorne, 2012: Assessing the value of Microwave Sounding Unit-radiosonde comparisons in ascertaining errors in climate data records of tropospheric temperatures. J. Geophys. Res. Atmos., 117, D19103. Mears, C. A., F. J. Wentz, P. Thorne, and D. Bernie, 2011: Assessing uncertainty in estimates of atmospheric temperature changes from MSU and AMSU using a Monte-Carlo estimation technique. J. Geophys. Res. Atmos., 116. Mears, C. A., C. E. Forest, R. W. Spencer, R. S. Vose, and R. W. Reynolds, 2006: What is our understanding of the contribution made by observational or methodological uncertainties to the previously reported vertical differences in temperature trends? In: Temperature Trends in the Lower Tmosphere: Steps for Understanding and Reconciling Differences [T. R. Karl, S. J. Hassol, C. D. Miller, and W. L. Murray (eds.)], 71-88. Mears, C. A., B. D. Santer, F. J. Wentz, K. E. Taylor, and M. F. Wehner, 2007: Relationship between temperature and precipitable water changes over tropical oceans. Geophys. Res. Lett., 34, L24709. Meehl, G. A., J. M. Arblaster, and G. Branstator, 2012: Mechanisms contributing to the warming hole and the consequent U.S. East–West differential of heat extremes. J. Clim., 25, 6394–6408. Mekis, É., and L. A. Vincent, 2011: An overview of the second generation adjusted daily precipitation dataset for trend analysis in Canada. Atmosphere-Ocean, 49, 163–177. Meng, Q. J., M. Latif, W. Park, N. S. Keenlyside, V. A. Semenov, and T. Martin, 2012: Twentieth century Walker Circulation change: Data analysis and model experiments. Clim. Dyn., 38, 1757–1773. Menne, M. J., and C. N. Williams, 2009: Homogenization of temperature series via pairwise comparisons. J. Clim., 22, 1700–1717. Menne, M. J., C. N. Williams, and M. A. Palecki, 2010: On the reliability of the US surface temperature record. J. Geophys. Res. Atmos., 115, D11108. Menzel, W. P., 2001: Cloud tracking with satellite imagery: From the pioneering work of Ted Fujita to the present. Bull. Am. Meteor. Soc., 82, 33–47. Merchant, C. J., et al., 2012: A 20 year independent record of sea surface temperature for climate from Along Track Scanning Radiometer. J. Geophys. Res., 117. C12013. Merrifield, M. A., 2011: A shift in western tropical Pacific sea level trends during the 1990s. J. Clim., 24, 4126–4138. Mezher, R. N., M. Doyle, and V. Barros, 2012: Climatology of hail in Argentina. Atmos. Res., 114–115, 70–82. Mieruch, S., S. Noel, H. Bovensmann, and J. P. Burrows, 2008: Analysis of global water vapour trends from satellite measurements in the visible spectral range. Atmos. Chem. Phys., 8, 491–504. Milewska, E. J., 2004: Baseline cloudiness trends in Canada 1953–2002. Atmos. Ocean, 42, 267–280. Miller, B., et al., 2010: HFC-23 (CHF3) emission trend response to HCFC-22 (CHClF2) production and recent HFC-23 emission abatement measures. Atmos. Chem. Phys., 10, 7875–7890. Milliman, J. D., K. L. Farnsworth, P. D. Jones, K. H. Xu, and L. C. Smith, 2008: Climatic and anthropogenic factors affecting river diSchärge to the global ocean, 1951–2000. Global Planet. Change, 62, 187–194. Mills, T. C., 2010: ‘Skinning a cat’: Alternative models of representing temperature trends. Clim. Change, 101, 415–426. Milz, M., et al., 2005: Water vapor distributions measured with the Michelson Interferometer for passive atmospheric sounding on board Envisat (MIPAS/Envisat). J. Geophys. Res., 110, D24307. Mishchenko, M. I., et al., 2007: Long-term satellite record reveals likely recent aerosol trend. Science, 315, 1543–1543. Mishchenko, M. I., et al., 2012: Aerosol retrievals from channel-1 and -2 AVHRR radiances: Long-term trends updated and revisited. J. Quant. Spectr. Radiat. Trans., 113, 1974–1980. Misra, V., J. P. Michael, R. Boyles, E. P. Chassignet, M. Griffin, and J. J. O’Brien, 2012: Reconciling the spatial distribution of the surface temperature trends in the southeastern United States. J. Clim., 25, 3610–3618. Mitas, C. M., and A. Clement, 2005: Has the Hadley cell been strengthening in recent decades? Geophys. Res. Lett., 32, L030809. Mitchell, T. D., and P. D. Jones, 2005: An improved method of constructing a database of monthly climate observations and associated high-resolution grids. Int. J. Climatol., 25, 693–712. Mo, K., and J. Paegle, 2001: The Pacific-South American modes and their downstream effects. Int. J. Climatol., 21, 1211–1229. Moberg, A., et al., 2006: Indices for daily temperature and precipitation extremes in Europe analyzed for the period 1901–2000. J. Geophys. Res. Atmos., 111, D22106. Mohapatra, M., B. K. Mandyopadhyay, and A. Tyagi, 2011: Best track parameters of tropical cyclones over the North Indian Ocean: A review. Natural Hazards, 63, 1285-1317. Mokhov, I. I., M. G. Akperov, M. A. Prokofyeva, A. V. Timazhev, A. R. Lupo, and H. Le Treut, 2013: Blockings in the Northern Hemisphere and Euro-Atlantic region: Estimates of changes from reanalyses data and model simulations. Doklady, Earth Sci., 449, 430-433. Monaghan, A. J., and D. H. Bromwich, 2008: Advances describing recent Antarctic climate variability. Bull. Am. Meteorol. Soc., 89, 1295–1306. Monaghan, A. J., D. H. Bromwich, W. Chapman, and J. C. Comiso, 2008: Recent variability and trends of Antarctic near-surface temperature. J. Geophys. Res. Atmos., 113, D04105. Monk, W., D. L. Peters, D. J. Baird, and R. A. Curry, 2011: Trends in indicator hydrological variables for Canadian rivers. Hydrol. Proc., 25, 3086–3100. Monks, P. S., et al., 2009: Atmospheric composition change – global and regional air quality. Atmos. Environ., 43, 5268–5350. Montzka, S., B. Hall, and J. Elkins, 2009: Accelerated increases observed for hydrochlorofluorocarbons since 2004 in the global atmosphere. Geophys. Res. Lett., 36, L03804 . Montzka, S., M. Krol, E. Dlugokencky, B. Hall, P. Jockel, and J. Lelieveld, 2011: Small interannual variability of global atmospheric hydroxyl. Science, 331, 67-69. Montzka, S., L. Kuijpers, M. Battle, M. Aydin, K. Verhulst, E. Saltzman, and D. Fahey, 2010: Recent increases in global HFC-23 emissions. Geophys. Res. Lett., 37, L02808. Montzka, S. A., et al., 2011b: Ozone-depleting substances (ODSs) and related chemicals. In Scientific Assessment of Ozone Depletion: 2010, Global Ozone Research and Monitoring Project—Report No. 52. World Meteorological Organization, Geneva, Switzerland, 516 pp. Morak, S., G. C. Hegerl, and J. Kenyon, 2011: Detectable regional changes in the number of warm nights. Geophys. Res. Lett., 38, 5. Morak, S., G. C. Hegerl, and N. Christidis, 2013: Detectable changes in the frequency of temperature extremes. J. Clim., 26, 1561–1574. Morice, C. P., J. J. Kennedy, N. A. Rayner, and P. D. Jones, 2012: Quantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: The HadCRUT4 data set. J. Geophys. Res. Atmos., 117, 22. Mueller, B., and S. Seneviratne, 2012: Hot days induced by precipitation deficits at the global scale. Proc. Natl. Acad. Sci. U.S.A., 109, 12398-12403. Mueller, B., et al., 2011: Evaluation of global observations-based evapotranspiration datasets and IPCC AR4 simulations. Geophys. Res. Lett., 38, L06402. Muhle, J., et al., 2010: Perfluorocarbons in the global atmosphere: tetrafluoromethane, hexafluoroethane, and octafluoropropane. Atmos. Chem. Phys., 10, 5145- 5164. Murphy, D. M., et al., 2011: Decreases in elemental carbon and fine particle mass in the United States. Atmos. Chem. Phys., 11, 4679–4686. Nan, S., and J. P. Li, 2003: The relationship between the summer precipitation in the Yangtze River Valley and the boreal spring Southern Hemisphere annular mode. Geophys. Res. Lett., 30, 2266. Nash, J., and P. R. Edge, 1989: Temperature changes in the stratosphere and lower mesosphere 197–1988 inferred from TOVS radiance observations. Adv. Space Res., 9, 333–341. Neff, W., J. Perlwitz, and M. Hoerling, 2008: Observational evidence for asymmetric changes in tropospheric heights over Antarctica on decadal time scales. Geophys. Res. Lett., 35, L18703. Neu, U., et al., 2012: IMILAST: A community effort to intercompare extratropical cyclone detection and tracking algorithms. Bull. Am. Meteor. Soc., 94, 529–547. Nevison, C., et al., 2011: Exploring causes of interannual variability in the seasonal cycles of tropospheric nitrous oxide. Atmos. Chem. Phys., 11, 3713–3730. New, M., et al., 2006: Evidence of trends in daily climate extremes over southern and west Africa. J. Geophys. Res. Atmos., 111, D14102. Nguyen, H., B. Timbal, I. Smith, A. Evans, and C. Lucas, 2013: The Hadley circulation in reanalyses: Climatology, variability and change. J. Clim., 26, 3357–3376. Nicholls, N., 2008: Recent trends in the seasonal and temporal behaviour of the El Niño-Southern Oscillation. Geophys. Res. Lett., 35, L19703. Nisbet, E., and R. Weiss, 2010: Top-down versus bottom-up. Science, 328, 1241- 1243. Norris, J. R., and M. Wild, 2007: Trends in aerosol radiative effects over Europe inferred from observed cloud cover, solar “dimming” and solar “brightening”. J. Geophys. Res. Atmos., 112, D08214. Norris, J. R., and M. Wild, 2009: Trends in aerosol radiative effects over China and Japan inferred from observed cloud cover, solar dimming, and solar brightening. J. Geophys. Res. Atmos., 114, D00d15. O’Dell, C. W., F. J. Wentz, and R. Bennartz, 2008: Cloud liquid water path from satellite-based passive microwave observations: A new climatology over the global oceans. J. Clim., 21, 1721–1739. O’Doherty, S., et al., 2009: Global and regional emissions of HFC-125 (CHF2CF3) from in situ and air archive atmospheric observations at AGAGE and SOGE observatories. J. Geophys. Res. Atmos., 109, D06310. O’Donnell, R., N. Lewis, S. McIntyre, and J. Condon, 2011: Improved methods for PCA-based reconstructions: Case study using the Steig et al. (2009) Antarctic Temperature Reconstruction. J. Clim., 24, 2099–2115. O’Gorman, P., R. P. Allan, M. P. Byrne, and M. Previdi, 2012: Energentic constraints on precipitation under climate change. Surv. Geophys., 33, 585–608. Ohmura, A., 2009: Observed decadal variations in surface solar radiation and their causes. J. Geophys. Res. Atmos., 114, D00d05. Ohmura, A., et al., 1998: Baseline Surface Radiation Network (BSRN/WCRP): New precision radiometry for climate research. Bull. Am. Meteor. Soc., 79, 2115–2136. Ohvril, H., et al., 2009: Global dimming and brightening versus atmospheric column transparency, Europe, 1906–2007. J. Geophys. Res. Atmos., 114, D00d12. Oltmans, S. J., et al., 2013: Recent tropospheric ozone changes – A pattern dominated by slow or no growth. Atmos. Environ., 67, 331–351. Onogi, K., et al., 2007: The JRA-25 reanalysis. J. Meteorol. Soc. Jpn., 85, 369–432. Oort, A. H., and J. J. Yienger, 1996: Observed interannual variability in the Hadley circulation and its connection to ENSO. J. Clim., 9, 2751–2767. Osborn, T. J., 2011: Winter 2009/2010 temperatures and a record breaking North Atlantic Oscillation index. Weather, 66, 19–21. Paciorek, C. J., J. S. Risbey, V. Ventura, and R. D. Rosen, 2002: Multiple indices of Northern Hemisphere cyclone activity, winters 1949–99. J. Clim., 15, 1573–1590. Palmer, M. D., K. Haines, S. F. B. Tett, and T. J. Ansell, 2007: Isolating the signal of ocean global warming. Geophys. Res. Lett., 34, 6. Palmer, W. C., 1965: Meteorological drought. US Weather Bureau Research Paper, 45, 58 pages. Paltridge, G., A. Arking, and M. Pook, 2009: Trends in middle- and upper-level tropospheric humidity from NCEP reanalysis data. Theor. Appl. Climatol., 98, 351–359. Pan, Z. T., R. W. Arritt, E. S. Takle, W. J. Gutowski, C. J. Anderson, and M. Segal, 2004: Altered hydrologic feedback in a warming climate introduces a ‘‘warming hole’’. Geophys. Res. Lett., 31, L17109. Panagiotopoulos, F., M. Shahgedanova, A. Hannachi, and D. B. Stephenson, 2005: Observed trends and teleconnections of the Siberian high: A recently declining center of action. J. Clim., 18, 1411–1422. Parker, D., C. Folland, A. Scaife, J. Knight, A. Colman, P. Baines, and B. Dong, 2007: Decadal to multidecadal variability and the climate change background. J. Geophys. Res. Atmos., 112. D18115. Parker, D. E., 2006: A demonstration that large-scale warming is not urban. J. Clim., 19, 2882–2895. Parker, D. E., 2011: Recent land surface air temperature trends assessed using the 20th century reanalysis. J. Geophys. Res. Atmos., 116, D20125. Parker, D. E., P. Jones, T. C. Peterson, and J. Kennedy, 2009: Comment on “Unresolved issues with the assessment of multidecadal global land surface temperature trends” by Roger A. Pielke Sr. et al. J. Geophys. Res. Atmos., 114. D05104. Parrish, D. D., et al., 2012: Long-term changes in lower tropospheric baseline ozone concentrations at northern mid-latitudes. Atmos. Chem. Phys., 12, 11485–11504. Pattanaik, D. R., and M. Rajeevan, 2010: Variability of extreme rainfall events over India during southwest monsoon season. Meteorol. Appl., 17, 88–104. Pavan, V., R. Tomozeiu, C. Cacciamani, and M. Di Lorenzo, 2008: Daily precipitation observations over Emilia-Romagna: Mean values and extremes. Int. J. Climatol., 28, 2065–2079. Pavelin, E. G., C. E. Johnson, S. Rughooputh, and R. Toumi, 1999: Evaluation of pre-industrial surface ozone measurements made using Sch\onbein’s method. Atmos. Environ., 33, 919–929. Perkins, S. E., and L. V. Alexander, 2012: On the measurement of heat waves. J. Clim., 26, 4500-4517 . Perkins, S. E., L. V. Alexander, and J. R. Nairn, 2012: Increasing frequency, intensity and duration of observed global heatwaves and warm spells. Geophys. Res. Lett., 39. L20714. Peterson, T. C., K. M. Willett, and P. W. Thorne, 2011: Observed changes in surface atmospheric energy over land. Geophys. Res. Lett., 38, L16707. Peterson, T. C., X. B. Zhang, M. Brunet-India, and J. L. Vazquez-Aguirre, 2008: Changes in North American extremes derived from daily weather data. J. Geophys. Res. Atmos., 113, D07113. Peterson, T. C., et al., 2009: State of the Climate in 2008. Bull. Am. Meteor. Soc., 90, S13-. Peterson, T. C., et al., 2013: Monitoring and understanding changes in heat waves, cold waves, floods and droughts in the United States: State of knowledge. Bull. Am. Meteor. Soc., 94, 821-834. Petrow, T., and B. Merz, 2009: Trends in flood magnitude, frequency and seasonality in Germany in the period 1951–2002. J. Hydrol., 371, 129–141. Pezza, A., P. van Rensch, and W. Cai, 2012: Severe heat waves in Southern Australia: Synoptic climatology and large scale connections. Clim. Dyn., 38, 209–224. Pezza, A. B., I. Simmonds, and J. A. Renwick, 2007: Southern Hemisphere cyclones and anticyclones: Recent trends and links with decadal variability in the Pacific Ocean. Int. J. Climatol., 27, 1403–1419. Philipona, R., 2012: Greenhouse warming and solar brightening in and around the Alps. Int. J. Climatol., 33, 1530-1537. Philipona, R., K. Behrens, and C. Ruckstuhl, 2009: How declining aerosols and rising greenhouse gases forced rapid warming in Europe since the 1980s. Geophys. Res. Lett., 36, L02806. Philipona, R., B. Dürr, A. Ohmura, and C. Ruckstuhl, 2005: Anthropogenic greenhouse forcing and strong water vapor feedback increase temperature in Europe. Geophys. Res. Lett., 32, L19809. Philipona, R., B. Dürr, C. Marty, A. Ohmura, and M. Wild, 2004: Radiative forcingmeasured at Earth’s surface—corroborate the increasing greenhouse effect. Geophys. Res. Lett., 31, L03202. Philipp, A., P. M. Della-Marta, J. Jacobeit, D. R. Fereday, P. D. Jones, A. Moberg, and H. Wanner, 2007: Long-term variability of daily North Atlantic-European pressure patterns since 1850 classified by simulated annealing clustering. J. Clim., 20, 4065–4095. Piao, S., et al., 2010: The impacts of climate change on water resources and agriculture in China. Nature, 467, 43–51. Pielke, R. A., and T. Matsui, 2005: Should light wind and windy nights have the same temperature trends at individual levels even if the boundary layer averaged heat content change is the same? Geophys. Res. Lett., 32, L21813. Pielke, R. A., Sr., et al., 2007: Unresolved issues with the assessment of multidecadal global land surface temperature trends. J. Geophys. Res. Atmos., 112, D24S08. Pinker, R. T., B. Zhang, and E. G. Dutton, 2005: Do satellites detect trends in surface solar radiation? Science, 308, 850–854. Pirazzoli, P. A., and A. Tomasin, 2003: Recent near-surface wind changes in the central Mediterranean and Adriatic areas. Int. J. Climatol., 23, 963–973. Po-Chedley, S., and Q. Fu, 2012: A bias in the Midtropospheric Channel Warm Target Factor on the NOAA-9 Microwave Sounding Unit. J. Atmos. Ocean Technol., 29, 646–652. Portmann, R., S. Solomon, and G. Hegerl, 2009a: Spatial and seasonal patterns in climate change, temperatures, and precipitation across the United States. Proc. Natl. Acad. Sci. U.S.A., 106, 7324–7329. Portmann, R. W., S. Solomon, and G. C. Hegerl, 2009b: Linkages between climate change, extreme temperature and precipitation across the United States. Proc. Natl. Acad. Sci. U.S.A., 106, 7324–7329. Power, S., T. Casey, C. Folland, A. Colman, and V. Mehta, 1999: Inter-decadal modulation of the impact of ENSO on Australia. Clim. Dyn., 15, 319–324. Power, S. B., and G. Kociuba, 2011a: The impact of global warming on the Southern Oscillation Index. Clim. Dynamics, 37, 1745–1754. Power, S. B., and G. Kociuba, 2011b: What caused the observed twentieth-century weakening of the Walker Circulation? J. Clim., 24, 6501–6514. Pozzoli, L., et al., 2011: Reanalysis of tropospheric sulfate aerosol and ozone for the period 1980–2005 using the aerosol-chemistry-climate model ECHAM5– HAMMOZ. Atmos. Chem. Phys., 11, 9563–9594. Prata, F., 2008: The climatological record of clear-sky longwave radiation at the Earth’s surface: Evidence for water vapour feedback? Int. J. Remote Sens., 29, 5247–5263. Prather, M., C. Holmes, and J. Hsu, 2012: Reactive greenhouse gas scenarios: Systematic exploration of uncertainties and the role of atmospheric chemistry. Geophys. Res. Lett., 39, L09803. Prinn, R., et al., 2005: Evidence for variability of atmospheric hydroxyl radicals over the past quarter century. Geophys. Res. Lett., L07809. Pryor, S. C., R. J. Barthelmie, and E. S. Riley, 2007: Historical evolution of wind climates in the USA - art. no. 012065. In: Science of Making Torque from Wind [M. O. L. Hansen and K. S. Hansen (eds.)], 75, 12065–12065. Pryor, S. C., J. A. Howe, and K. E. Kunkel, 2009: How spatially coherent and statistically robust are temporal changes in extreme precipitation in the contiguous USA? Int. J. Climatol., 29, 31–45. Qian, Y., D. P. Kaiser, L. R. Leung, and M. Xu, 2006: More frequent cloud-free sky and less surface solar radiation in China from 1955 to 2000. Geophys. Res. Lett., 33, L01812. Qian, Y., W. G. Wang, L. R. Leung, and D. P. Kaiser, 2007: Variability of solar radiation under cloud-free skies in China: The role of aerosols. Geophys. Res. Lett., 34, L12804. Qian, Y., D. Gong, J. Fan, L. Leung, R. Bennartz, D. Chen, and W. Wang, 2009: Heavy pollution suppresses light rain in China: Observations and modeling. J. Geophys. Res. Atmos., 114, D00K02. Rahimzadeh, F., A. Asgari, and E. Fattahi, 2009: Variability of extreme temperature and precipitation in Iran during recent decades. Int. J. Climatol., 29, 329–343. Raible, C. C., P. M. Della-Marta, C. Schwierz, H. Wernli, and R. Blender, 2008: Northern hemisphere extratropical cyclones: A comparison of detection and tracking methods and different reanalyses. Mon. Weather Rev., 136, 880–897. Raichijk, C., 2011: Observed trends in sunshine duration over South America. Int. J. Climatol., 32, 669-680. Randall, R. M., and B. M. Herman, 2008: Using limited time period trends as a means to determine attribution of discrepancies in microwave sounding unit-derived tropospheric temperature time series. J. Geophys. Res. Atmos., 113, D05105. Randel, W. J., 2010: Variability and trends in stratospheric temperature and water vapor. The Stratosphere: Dynamics, Transport and Chemistry, S. Polvani, and Waugh, Ed., American Geophysical Union, 123–135. Randel, W. J., and E. J. Jensen, 2013: Physical processes in the tropical tropopause layer and their roles in a changing climate. Nature Geosci., 169–176. Randel, W. J., F. Wu, H. Vömel, G. E. Nedoluha, and P. Forster, 2006: Decreases in stratospheric water vapor after 2001: Links to changes in the tropical tropopause and the Brewer-Dobson circulation. J. Geophys. Res. Atmos., 111, D12312. Randel, W. J., et al., 2009: An update of observed stratospheric temperature trends. J. Geophys. Res. Atmos., 114, D02107. Rasmusson, E. M., and T. H. Carpenter, 1982: Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/El Niño. Mon. Weather Rev., 110, 354–384. Rasmusson, E. M., and J. M. Wallace, 1983: Meteorological aspects of the El NiñoSouthern Oscillation. Science, 222, 1195–1202. Rausch, J., A. Heidinger, and R. Bennartz, 2010: Regional assessment of microphysical properties of marine boundary layer cloud using the PATMOS-x dataset. J. Geophys. Res. Atmos., 115, D23212. Ray, E. A., et al., 2010: Evidence for changes in stratospheric transport and mixing over the past three decades based on multiple data sets and tropical leaky pipe analysis. J. Geophys. Res. Atmos., 115, D21304. Rayner, D. P., 2007: Wind run changes: The dominant factor affecting pan evaporation trends in Australia. J. Clim., 20, 3379–3394. Rayner, N. A., et al., 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res. Atmos., 108, 37. Rayner, N. A., et al., 2006: Improved analyses of changes and uncertainties in sea surface temperature measured in situ sice the mid-nineteenth century: The HadSST2 dataset. J. Clim., 19, 446–469. Read, W. G., et al., 2007: Aura Microwave Limb Sounder upper tropospheric and lower stratospheric H2O and relative humidity with respect to ice validation. J. Geophys. Res. Atmos., 112, D24S35. Ren, G., et al., 2011: Change in climatic extremes over mainland China based on an integrated extreme climate index. Clim. Res., 50, 113–124. Ren, G. Y., Z. Y. Chu, Z. H. Chen, and Y. Y. Ren, 2007: Implications of temporal change in urban heat island intensity observed at Beijing and Wuhan stations. Geophys. Res. Lett., 34, L05711. Ren, G. Y., Y. Q. Zhou, Z. Y. Chu, J. X. Zhou, A. Y. Zhang, J. Guo, and X. F. Liu, 2008: Urbanization effects on observed surface air temperature trends in north China. J. Clim., 21, 1333–1348. Ren, H.-L., and F.-F. Jin, 2011: Niño indices for two types of ENSO. Geophys. Res. Lett., 38, L04704. Ren, Y. Y., and G. Y. Ren, 2011: A remote-sensing method of selecting reference stations for evaluating urbanization effect on surface air temperature trends. J. Clim., 24, 3179–3189. Renard, B., et al., 2008: Regional methods for trend detection: Assessing field significance and regional consistency. Water Resourc. Res., 44, W08419. Revadekar, J., D. Kothawale, S. Patwardhan, G. Pant, and K. Kumar, 2012: About the observed and future changes in temperature extremes over India. Nat. Hazards, 60, 1133–1155. Reynolds, R., N. Rayner, T. Smith, D. Stokes, and W. Wang, 2002: An improved in situ and satellite SST analysis for climate. J. Clim., 15, 1609–1625. Reynolds, R. W., C. L. Gentemann, and G. K. Corlett, 2010: Evaluation of AATSR and TMI Satellite SST Data. J. Clim., 23, 152–165. Rhines, A., and P. Huybers, 2013: Frequent summer temperature extremes reflect changes in the mean, not the variance. Proc. Natl. Acad. Sci. U.S.A., 110, E546– E546. Rienecker, M. M., Suarez, M.J., Gelaro, R., Todling, R., Bacmeister, J., Liu, E., Bosilovich, M. G., Schubert, S. D., Takacs, L., Kim, G.-K., Bloom, S., Chen, J., Collins, D., Conaty, A., da Silva, A., Gu, W., Joiner, J., Koster, R. D., Lucchesi, R., Molod, A., Owens, T., Pawson, S., Pegion, P., Redder, C. R., Reichle, R., Robertson, F. R., Ruddick, A. G., Sienkiewicz, M., and Woollen, J., 2011: MERRA: NASA’s modernera retrospective analysis for research and applications. J. Clim., 24, 3624-3648. Rigby, M., et al., 2008: Renewed growth of atmospheric methane. Geophys. Res. Lett., 35, L22805. Rigby, M., et al., 2010: History of atmospheric SF6 from 1973 to 2008. Atmos. Chem. Phys., 10, 10305-10320. Riihimaki, L. D., F. E. Vignola, and C. N. Long, 2009: Analyzing the contribution of aerosols to an observed increase in direct normal irradiance in Oregon. J. Geophys. Res. Atmos., 114, D00d02. Robock, A., et al., 2000: The Global Soil Moisture Data Bank. Bull. Am. Meteor. Soc., 81, 1281–1299. Rockmann, T., and I. Levin, 2005: High-precision determination of the changing isotopic composition of atmospheric N2O from 1990 to 2002. J. Geophys. Res. Atmos., 110, D21304. Roderick, M. L., and G. D. Farquhar, 2002: The cause of decreased pan evaporation over the past 50 years. Science, 298, 1410–1411. Roderick, M. L., L. D. Rotstayn, G. D. Farquhar, and M. T. Hobbins, 2007: On the attribution of changing pan evaporation. Geophys. Res. Lett., 34, L17403. Rohde, R., et al., 2013a: A new estimate of the average Earth surface land temperature spanning 1753 to 2011. Geoinfor. Geostat.: An Overview, 1, doi:10.4172/ gigs.1000101. Rohde, R., et al., 2013b: Berkeley Earth temperature averaging process. Geoinfor Geostat: An Overview, 1, doi:10.4172/gigs.1000103. Rohs, S., et al., 2006: Long-term changes of methane and hydrogen in the stratosphere in the period 1978–2003 and their impact on the abundance of stratospheric water vapor. J. Geophys. Res. Atmos., 111, D14315. Ropelewski, C. F., and P. D. Jones, 1987: An extension of the Tahiti–Darwin Southern Oscillation Index. Mon. Weather Rev., 115, 2161–2165. Rosenlof, K. H., and G. C. Reid, 2008: Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection. J. Geophys. Res. Atmos., 113, D06107. Ruckstuhl, C., et al., 2008: Aerosol and cloud effects on solar brightening and the recent rapid warming. Geophys. Res. Lett., 35, L12708. Ruddiman, W., 2003: The anthropogenic greenhouse era began thousands of years ago. Clim. Change, 261–293. Ruddiman, W., 2007: The early anthropogenic hypothesis: Challenges and responses. Rev. Geophys., 45, RG4001. Russak, V., 2009: Changes in solar radiation and their influence on temperature trend in Estonia (1955–2007). J. Geophys. Res. Atmos., 114, D00d01. Russell, A. R., L. C. Valin, E. J. Bucsela, M. O. Wenig, and R. C. Cohen, 2010: Spacebased constraints on spatial and temporal patterns of NOx emissions in California, 2005−2008. Environ. Sci. Technol., 44, 3608–3615. Russell, J., et al., 1993: The halogen occultation experiment. J. Geophys. Res. Atmos., 98, 10777–10797. Rusticucci, M., and M. Renom, 2008: Variability and trends in indices of quality-controlled daily temperature extremes in Uruguay. Int. J. Climatol., 28, 1083–1095. Saha, S., et al., 2010: The NCEP climate forecaset system reanalysis. Bull. Am. Meteor. Soc., 91, 1015–1057. Saikawa, E., et al., 2012: Global and regional emissions estimates for HCFC-22. Atmos. Chem. Phys. Discuss., 12, 18423–18285. Saji, N. H., B. N. Goswami, P. N. Vinayachandran, and T. Yamagata, 1999: A dipole mode in the tropical Indian Ocean. Nature, 401, 360–363. Sakamoto, M., and J. R. Christy, 2009: The influences of TOVS radiance assimilation on temperature and moisture tendencies in JRA-25 and ERA-40. J. Atmos. Ocean Technol., 26, 1435–1455. Sanchez-Lorenzo, A., and M. Wild, 2012: Decadal variations in estimated surface solar radiation over Switzerland since the late 19th century. Atmos. Chem. Phys. Discussion, 12, 10815–10843. Sanchez-Lorenzo, A., J. Calbo, and J. Martin-Vide, 2008: Spatial and temporal trends in sunshine duration over Western Europe (1938–2004). J. Clim., 21, 6089–6098. Sanchez-Lorenzo, A., J. Calbo, and M. Wild, 2013: Global and diffuse solar radiation in Spain: Building a homogeneous dataset and assessing their trends. Global Planet. Change, 100, 343–352. Sanchez-Lorenzo, A., J. Calbo, M. Brunetti, and C. Deser, 2009: Dimming/brightening over the Iberian Peninsula: Trends in sunshine duration and cloud cover and their relations with atmospheric circulation. J. Geophys. Res. Atmos., 114, D00d09. Santer, B., et al., 2008: Consistency of modelled and observed temperature trends in the tropical troposphere. Int. J. Climatol., 28, 1703–1722. Santer, B. D., et al., 2007: Identification of human-induced changes in atmospheric moisture content. Proc. Natl. Acad. Sci. U.S.A., 104, 15248–15253. Santer, B. D., et al., 2011: Separating signal and noise in atmospheric temperature changes: The importance of timescale. J. Geophys. Res. Atmos., 116, D22105. Scaife, A., C. Folland, L. Alexander, A. Moberg, and J. Knight, 2008: European climate extremes and the North Atlantic Oscillation. J. Clim., 21, 72–83. Schär, C., P. L. Vidale, D. Luthi, C. Frei, C. Haberli, M. A. Liniger, and C. Appenzeller, 2004: The role of increasing temperature variability in European summer heatwaves. Nature, 427, 332–336. Scherer, M., H. Vömel, S. Fueglistaler, S. J. Oltmans, and J. Staehelin, 2008: Trends and variability of midlatitude stratospheric water vapour deduced from the re-evaluated Boulder balloon series and HALOE. Atmos. Chem. Phys., 8, 1391–1402. Scherrer, S. C., and C. Appenzeller, 2006: Swiss Alpine snow pack variability: Major patterns and links to local climate and large-scale flow. Clim. Res., 32, 187–199. Scherrer, S. C., C. Wüthrich, M. Croci-Maspoli, R. Weingartner, and C. Appenzeller, 2013: Snow variability in the Swiss Alps 1864–2009. Int. J. Climatol., doi: 10.1002/joc.3653. Schiller, C., J. U. Grooss, P. Konopka, F. Plager, F. H. Silva dos Santos, and N. Spelten, 2009: Hydration and dehydration at the tropical tropopause. Atmos. Chem. Phys., 9, 9647–9660. Schmidt, G. A., 2009: Spurious correlations between recent warming and indices of local economic activity. Int. J. Climatol., 29, 2041–2048. Schnadt Poberaj, C., J. Staehelin, D. Brunner, V. Thouret, H. De Backer, and R. Stübi, 2009: Long-term changes in UT/LS ozone between the late 1970s and the 1990s deduced from the GASP and MOZAIC aircraft programs and from ozonesondes. Atmos. Chem. Phys., 9, 5343–5369. Schneider, T., P. A. O’Gorman, and X. J. Levine, 2010: Water vapour and the dynamics of climate changes. Rev. Geophys., RG3001. Schneidereit, A., R. Blender, K. Fraedrich, and F. Lunkeit, 2007: Icelandic climate and north Atlantic cyclones in ERA-40 reanalyses. Meteorol. Z., 16, 17–23. Schwartz, R. D., 2005: Global dimming: Clear-sky atmospheric transmission from astronomical extinction measurements. J. Geophys. Res. Atmos., 110. Scinocca, J. F., D. B. Stephenson, T. C. Bailey, and J. Austin, 2010: Estimates of past and future ozone trends from multimodel simulations using a flexible smoothing spline methodology. J. Geophys. Res. Atmos., 115. Screen, J. A., and I. Simmonds, 2011: Erroneous Arctic temperature trends in the ERA-40 reanalysis: A closer look. J. Clim., 24, 2620–2627. Seidel, D. J., and J. R. Lanzante, 2004: An assessment of three alternatives to linear trends for characterizing global atmospheric temperature changes. J. Geophys. Res. Atmos., 109, D14108. Seidel, D. J., and W. J. Randel, 2007: Recent widening of the tropical belt: Evidence from tropopause observations. J. Geophys. Res. Atmos., 112, D20113. Seidel, D. J., Q. Fu, W. J. Randel, and T. J. Reichler, 2008: Widening of the tropical belt in a changing climate. Nature Geosci., 1, 21–24. Seidel, D. J., N. P. Gillett, J. R. Lanzante, K. P. Shine, and P. W. Thorne, 2011: Stratospheric temperature trends: Our evolving understanding. Clim. Change, 2, 592–616. Sen Roy, S., 2009: A spatial analysis of extreme hourly precipitation patterns in India. Int. J. Climatol., 29, 345–355. Sen Roy, S., and R. C. Balling, 2005: Analysis of trends in maximum and minimum temperature, diurnal temperature range, and cloud cover over India. Geophys. Res. Lett., 32, L12702. Sen Roy, S., and M. Rouault, 2013: Spatial patterns of seasonal scale trends in extreme hourly precipitation in South Africa. Appl. Geogr., 39, 151–157. Seneviratne, S. I., et al., 2010: Investigating soil moisture-climate interactions in a changing climate: A review. Earth Sci. Rev., 99, 125–161. Seneviratne, S. I., et al., 2012: Changes in climate extremes and their impacts on the natural physical environment. In: IPCC Special Report on Extremes, 109-230. Serquet, G., C. Marty, J. P. Dulex, and M. Rebetez, 2011: Seasonal trends and temperature dependence of the snowfall/precipitation-day ratio in Switzerland. Geophys. Res. Lett., 38, L07703. Shaw, S. B., A. A. Royem, and S. J. Riha, 2011: The relationship between extreme hourly precipitation and surface temperature in different hydroclimatic regions of the United States. J. Hydrometeor., 12, 319–325. Sheffield, J., and E. F. Wood, 2008: Global trends and variability in soil moisture and drought characteristics, 1950–2000, from observation-driven simulations of the terrestrial hydrologic cycle. J. Clim., 21, 432–458. Sheffield, J., E. Wood, and M. Roderick, 2012: Little change in global drought over the past 60 years. Nature, 491, 435–. Sheffield, J., K. Andreadis, E. Wood, and D. Lettenmaier, 2009: Global and continental drought in the second half of the twentieth century: Severity-area-duration analysis and temporal variability of large-scale events. J. Clim., 22, 1962–1981. Shekar, M., H. Chand, S. Kumar, K. Srinivasan, and A. Ganju, 2010: Climate change studies in the western Himalaya. Ann. Glaciol., 51, 105-112. Sherwood, S. C., R. Roca, and T. M. Weckwerth, 2010: Tropospheric water vapor, convection, and climate. Rev. Geophys., 48, RG2001. Sherwood, S. C., C. L. Meyer, R. J. Allen, and H. A. Titchner, 2008: Robust tropospheric warming revealed by iteratively homogenized radiosonde data. J. Clim., 21, 5336–5350. Shi, G. Y., et al., 2008: Data quality assessment and the long-term trend of ground solar radiation in China. J. Appl. Meteor. Climatol., 47, 1006–1016. Shi, L., and J. J. Bates, 2011: Three decades of intersatellite-calibrated High-Resolution Infrared Radiation Sounder upper tropospheric water vapor. J. Geophys. Res. Atmos., 116, D04108. Shiklomanov, A. I., R. B. Lammers, M. A. Rawlins, L. C. Smith, and T. M. Pavelsky, 2007: Temporal and spatial variations in maximum river diSchärge from a new Russian data set. J. Geophys. Res. Biogeosci., 112. Shiklomanov, I. A., V. Y. Georgievskii, V. I. Babkin, and Z. A. Balonishnikova, 2010: Research problems of formation and estimation of water resources and water availability changes of the Russian Federation. Russ. Meteorol, Hydrol., 35, 13–19. Shiu, C. J., S. C. Liu, and J. P. Chen, 2009: Diurnally asymmetric trends of temperature, humidity, and precipitation in Taiwan. J. Clim., 22, 5635–5649. Sillmann, J., M. Croci-Maspoli, M. Kallache, and R. W. Katz, 2011: Extreme cold winter temperatures in Europe under the influence of North Atlantic atmospheric blocking. J. Clim., 24, 5899–5913. Simmons, A. J., K. M. Willett, P. D. Jones, P. W. Thorne, and D. P. Dee, 2010: Lowfrequency variations in surface atmospheric humidity, temperature, and precipitation: Inferences from reanalyses and monthly gridded observational data sets. J. Geophys. Res. Atmos., 115, D01110. Simolo, C., M. Brunetti, M. Maugeri, and T. Nanni, 2011: Evolution of extreme temperatures in a warming climate. Geophys. Res. Lett., 38, 6. Simpson, I. J., et al., 2012: Long-term decline of global atmospheric ethane concentrations and implications for methane. Nature, 488, 490–494. Skansi, M., et al., 2013: Warming and wetting signals emerging from analysis of changes in climate extreme indices over South America. Global Planet. Change, 100, 295–307. Skeie, R. B., T. K. Berntsen, G. Myhre, K. Tanaka, M. M. Kvalevåg, and C. R. Hoyle, 2011: Anthropogenic radiative forcing time series from pre-industrial times until 2010. Atmos. Chem. Phys., 11, 11827–11857. Smith, L. C., T. Pavelsky, G. MacDonald, I. A. Shiklomanov, and R. Lammers, 2007: Rising minimum daily flows in northern Eurasian rivers suggest a growing influence of groundwater in the high-latitude water cycle. J. Geophys. Res., 112, G04S47. Smith, T. M., and R. W. Reynolds, 2002: Bias corrections for historical sea surface temperatures based on marine air temperatures. J. Clim., 15, 73–87. Smith, T. M., T. C. Peterson, J. H. Lawrimore, and R. W. Reynolds, 2005: New surface temperature analyses for climate monitoring. Geophys. Res. Lett., 32, L14712. Smith, T. M., R. W. Reynolds, T. C. Peterson, and J. Lawrimore, 2008: Improvements to NOAA’s historical merged land-ocean surface temperature analysis (1880– 2006). J. Clim., 21, 2283–2296. Smith, T. M., P. A. Arkin, L. Ren, and S. S. P. Shen, 2012: Improved reconstruction of global precipitation since 1900. J. Atmos. Ocean. Technol., 29, 1505–1517. Smits, A., A. Tank, and G. P. Konnen, 2005: Trends in storminess over the Netherlands, 1962–2002. Int. J. Climatol., 25, 1331–1344. Sohn, B. J., and S. C. Park, 2010: Strengthened tropical circulations in past three decades inferred from water vapor transport. J. Geophys. Res. Atmos., 115, D15112. Solomon, S., K. Rosenlof, R. Portmann, J. Daniel, S. Davis, T. Sanford, and G. Plattner, 2010: Contributions of stratospheric water vapor to decadal changes in the rate of global warming. Science, 327, 1219-1223. Song, H., and M. H. Zhang, 2007: Changes of the boreal winter Hadley circulation in the NCEP-NCAR and ECMWF reanalyses: A comparative study. J. Clim., 20, 5191–5200. Soni, V. K., G. Pandithurai, and D. S. Pai, 2012: Evaluation of long-term changes of solar radiation in India. Int. J. Climatol., 32, 540–551. Sorteberg, A., and J. E. Walsh, 2008: Seasonal cyclone variability at 70 degrees N and its impact on moisture transport into the Arctic. Tellus A, 60, 570–586. Sousa, P., R. Trigo, P. Aizpurua, R. Nieto, L. Gimeno, and R. Garcia-Herrera, 2011: Trends and extremes of drought indices throughout the 20th century in the Mediterranean. Nat. Hazards Earth Syst. Sci., 11, 33–51. Spencer, R. W., and J. R. Christy, 1992: Precision and radiosonde validation of satellite gridpoint temperature anomalies. 2. A troposhperic retrieval and trends during 1979–90. J. Clim., 5, 858–866. St. Jacques, J.-M., and D. Sauchyn, 2009: Increasing winter baseflow and mean annual streamflow from possible permafrost thawing in the Northwest Territories, Canada. Geophys. Res. Lett., 36, L01401. Stachnik, J. P., and C. Schumacher, 2011: A comparison of the Hadley circulation in modern reanalyses. J. Geophys. Res. Atmos., 116, D22102. Stahl, K., and L. M. Tallaksen, 2012: Filling the white space on maps of European runoff trends: Estimates from a multi-model ensemble. Hydrol. Earth Syst. Sci. Discuss., 9, 2005–2032. Stahl, K., et al., 2010: Streamflow trends in Europe: Evidence from a dataset of nearnatural catchments. Hydrol. Earth Syst. Sci., 14, 2367–2382. Stanhill, G., and S. Cohen, 2001: Global dimming: A review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequences. Agr. Forest Meteorol., 107, 255–278. Steeneveld, G. J., A. A. M. Holtslag, R. T. McNider, and R. A. Pielke, 2011: Screen level temperature increase due to higher atmospheric carbon dioxide in calm and windy nights revisited. J. Geophys. Res. Atmos., 116. Stegall, S., and J. Zhang, 2012: Wind field climatology, changes, and extremes in the Chukchi-Beaufort Seas and Alaska North Slope during 1979–2009. J. Clim., 25, 8075–8089. Steig, E. J., D. P. Schneider, S. D. Rutherford, M. E. Mann, J. C. Comiso, and D. T. Shindell, 2009: Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year. Nature, 460, 766–766. Stenke, A., and V. Grewe, 2005: Simulation of stratospheric water vapor trends: Impact on stratospheric ozone chemistry. Atmos. Chem. Phys., 5, 1257–1272. Stephens, G. L., M. Wild, P. W. Stackhouse, T. L’Ecuyer, S. Kato, and D. S. Henderson, 2012a: The global character of the flux of downward longwave radiation. J. Clim., 25, 2329–2340. Stephens, G. L., et al., 2012b: An update on Earth’s energy balance in light of the latest global observations. Nature Geosci., 5, 691–696. Stephenson, D. B., H. F. Diaz, and R. J. Murnane, 2008: Definition, diagnosis and origin of extreme weather and climate events. In: Climate Extremes and Society [R. J. Murnane, and H. F. Diaz (eds.)] Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 11–23. Stern, D. I., 2006: Reversal of the trend in global anthropogenic sulfur emissions. Global Environ. Change Hum. Policy Dimens., 16, 207–220. Stickler, A., et al., 2010: The Comprehensive Historical Upper-Air Network. Bull. Am. Meteor. Soc., 91, 741–751. Stjern, C. W., J. E. Kristjansson, and A. W. Hansen, 2009: Global dimming and global brightening - an analysis of surface radiation and cloud cover data in northern Europe. Int. J. Climatol., 29, 643–653. Stohl, A., et al., 2009: An analytical inversion method for determining regional and global emissions of greenhouse gases: Sensitivity studies and application to halocarbons. Atmos. Chem. Phys., 1597–1620. Stohl, A., et al., 2010: Hydrochlorofluorocarbon and hydrofluorocarbon emissions in East Asia determined by inverse modeling. Atmos. Chem. Phys., 3545–3560. Streets, D. G., Y. Wu, and M. Chin, 2006: Two-decadal aerosol trends as a likely explanation of the global dimming/brightening transition. Geophys. Res. Lett., 33, L15806. Streets, D. G., et al., 2009: Anthropogenic and natural contributions to regional trends in aerosol optical depth, 1980–2006. J. Geophys. Res. Atmos., 114, D00D18. Strong, C., and R. E. Davis, 2007: Winter jet stream trends over the Northern Hemisphere. Q. J. R. Meteorol. Soc., 133, 2109–2115. Strong, C., and R. E. Davis, 2008: Comment on “Historical trends in the jet streams” by Cristina L. Archer and Ken Caldeira. Geophys. Res. Lett., L24806. Stubenrauch, C. J., et al., 2013: Assessment of global cloud datasets from satellite: Project and database initiated by the GEWEX radiation panel. Bull. Am. Meteorol. Soc., 94, 1031-1049. Sun, B. M., A. Reale, D. J. Seidel, and D. C. Hunt, 2010: Comparing radiosonde and COSMIC atmospheric profile data to quantify differences among radiosonde types and the effects of imperfect collocation on comparison statistics. J. Geophys. Res. Atmos., 115, D23104. Swart, N. C., and J. C. Fyfe, 2012: Observed and simulated changes in the Southern Hemisphere surface westerly wind-stress. Geophys. Res. Lett., 39, L16711. Syakila, A., and C. Kroeze, 2011: The global nitrous oxide budget revisited. Greenhouse Gas Meas. Management, 1, 17–26. Takahashi, K., A. Montecinos, K. Goubanova, and B. Dewitte, 2011: ENSO regimes: Reinterpreting the canonical and Modoki El Niño. Geophys. Res. Lett., 38, L10704. Takeuchi, Y., Y. Endo, and S. Murakami, 2008: High correlation between winter precipitation and air temperature in heavy-snowfall areas in Japan. Ann. Glaciol., 49, 7–10. Tang, G., Y. Ding, S. Wang, G. Ren, H. Liu, and L. Zhang, 2010: Comparative analysis of China surface air temperature series for the past 100 years. Adv. Climate Change Res., 1, 11–19. Tang, W. J., K. Yang, J. Qin, C. C. K. Cheng, and J. He, 2011: Solar radiation trend across China in recent decades: a revisit with quality-controlled data. Atmos. Chem. Phys., 11, 393–406. Tank, A., et al., 2006: Changes in daily temperature and precipitation extremes in central and south Asia. J. Geophys. Res. Atmos., 111, D16105. Tans, P., 2009: An accounting of the observed increase in oceanic and atmospheric CO2 and an outlook for the future. Oceanography, 26–35. Tarasova, O. A., I. A. Senik, M. G. Sosonkin, J. Cui, J. Staehelin, and A. S. H. Prévôt, 2009: Surface ozone at the Caucasian site Kislovodsk High Mountain Station and the Swiss Alpine site Jungfraujoch: Data analysis and trends (1990–2006). Atmos. Chem. Phys., 9, 4157–4175. Tegtmeier, S., K. Kruger, I. Wohltmann, K. Schoellhammer, and M. Rex, 2008: Variations of the residual circulation in the Northern Hemispheric winter. J. Geophys. Res. Atmos., 113, D16109. Teuling, A. J., et al., 2009: A regional perspective on trends in continental evaporation. Geophys. Res. Lett., 36, L02404. Thomas, B., E. Kent, V. Swail, and D. Berry, 2008: Trends in ship wind speeds adjusted for observation method and height. Int. J. Climatol., 28, 747–763. Thomas, G. E., et al., 2010: Validation of the GRAPE single view aerosol retrieval for ATSR-2 and insights into the long term global AOD trend over the ocean. Atmos. Chem. Phys., 10, 4849–4866. Thompson, D. W. J., and J. M. Wallace, 1998: The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophys. Res. Lett., 25, 1297–1300. Thompson, D. W. J., and J. M. Wallace, 2000: Annular modes in the extratropical circulation. Part I: Month-to-month variability. J. Clim., 13, 1000–1016. Thompson, D. W. J., J. J. Kennedy, J. M. Wallace, and P. D. Jones, 2008: A large discontinuity in the mid-twentieth century in observed global-mean surface temperature. Nature, 453, 646–649. Thompson, D. W. J., et al., 2012: The mystery of recent stratospheric temperature trends. Nature, 491, 692–697. Thorne, P. W., 2008: Arctic tropospheric warming amplification? Nature, 455, E1–E2. Thorne, P. W., and R. S. Vose, 2010: Reanalyses suitable for characterizing long-term trends: Are They Really Achievable? Bull. Am. Meteor. Soc., 91, 353–. Thorne, P. W., D. E. Parker, S. F. B. Tett, P. D. Jones, M. McCarthy, H. Coleman, and P. Brohan, 2005: Revisiting radiosonde upper air temperatures from 1958 to 2002. J. Geophys. Res. Atmos., 110. Thorne, P. W., et al., 2011: A quantification of uncertainties in historical tropical tropospheric temperature trends from radiosondes. J. Geophys. Res. Atmos., 116, D12116. Tietavainen, H., H. Tuomenvirta, and A. Venalainen, 2010: Annual and seasonal mean temperatures in Finland during the last 160 years based on gridded temperature data. Int. J. Climatol., 30, 2247–2256. Titchner, H. A., P. W. Thorne, M. P. McCarthy, S. F. B. Tett, L. Haimberger, and D. E. Parker, 2009: Critically reassessing tropospheric temperature trends from radiosondes using realistic validation experiments. J. Clim., 22, 465–485. Tokinaga, H., and S.-P. Xie, 2011a: Wave and anemometer-based sea surface wind (WASWind) for climate change analysis. J. Clim., 267-285. Tokinaga, H., and S. P. Xie, 2011b: Weakening of the equatorial Atlantic cold tongue over the past six decades. Nature Geosci., 4, 222-226. Tokinaga, H., S. P. Xie, A. Timmermann, S. McGregor, T. Ogata, H. Kubota, and Y. M. Okumura, 2012: Regional patterns of tropical Indo-Pacific climate change: Evidence of the Walker circulation weakening. J. Clim., 25, 1689–1710. Toreti, A., E. Xoplaki, D. Maraun, F. G. Kuglitsch, H. Wanner, and J. Luterbacher, 2010: Characterisation of extreme winter precipitation in Mediterranean coastal sites and associated anomalous atmospheric circulation patterns. Nat. Hazards Earth Syst. Sci., 10, 1037–1050. Torseth, K., et al., 2012: Introduction to the European Monitoring and Evaluation Programme (EMEP) and observed atmospheric composition change during 1972–2009. Atmos. Chem. Phys. Discuss., 12, 1733–1820. Trenberth, K., 2011: Changes in precipitation with climate change. Clim. Res., 47, 123–138. Trenberth, K., and J. Fasullo, 2012a: Climate extremes and climate change: The Russian heat wave and other climate extremes of 2010. J. Geophys. Res. Atmos., 117, D17103. Trenberth, K. E., 1984: Signal versus noise in the Southern Oscillation. Mon. Weather Rev., 112, 326–332. Trenberth, K. E., 1997: The definition of El Niño. Bull. Am. Meteor. Soc., 78, 2771– 2777. Trenberth, K. E., and D. A. Paolino, 1980: The Northern Hemisphere Sea-Level Pressure Data Set – Trends, errors, and discontinuities. Mon. Weather Rev., 108, 855–872. Trenberth, K. E., and J. W. Hurrell, 1994: Decadal atmosphere-ocean variations in the Pacific. Clim. Dyn., 9, 303–319. Trenberth, K. E., and T. J. Hoar, 1996: The 1990–1995 El Niño Southern Oscillation event: Longest on record. Geophys. Res. Lett., 23, 57–60. Trenberth, K. E., and D. P. Stepaniak, 2001: Indices of El Niño evolution. J. Clim., 14, 1697–1701. Trenberth, K. E., and D. J. Shea, 2006: Atlantic hurricanes and natural variability in 2005. Geophys. Res. Lett., 33, L12704. Trenberth, K. E., and J. T. Fasullo, 2010: Climate change tracking Earth’s energy. Science, 328, 316–317. Trenberth, K. E., and J. T. Fasullo, 2012b: Tracking Earth’s energy: From El Niño to global warming. Surv. Geophys., 33, 413–426. Trenberth, K. E., J. T. Fasullo, and J. Kiehl, 2009: Earth’s Global energy budget. Bull. Am. Meteor. Soc., 90, 311. Trenberth, K. E., J. T. Fasullo, and J. Mackaro, 2011: Atmospheric moisture transports from ocean to land and global energy flows in reanalyses. J. Clim., 24, 4907– 4924. Trenberth, K. E., et al., 2007: Observations: Surface and atmospheric climate change. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor and H. L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Trewin, B., 2012: A daily homogenized temperature data set for Australia. Int. J. Climatol., 33, 1510-1529. Trnka, M., J. Kysely, M. Mozny, and M. Dubrovsky, 2009: Changes in Central-European soil-moisture availability and circulation patterns in 1881–2005. Int. J. Climatol., 29, 655–672. Troccoli, A., K. Muller, P. Coppin, R. Davy, C. Russell, and A. L. Hirsch, 2012: Long-term wind speed trends over Australia. J. Climate, 25, 170–183. Troup, A. J., 1965: Southern Oscillation. Q. J. R. Meteorol. Soc., 91, 490–. Tryhorn, L., and J. Risbey, 2006: On the distribution of heat waves over the Australian region. Aust. Meteorol. Mag., 55, 169–182. Tung, K.-K., and J. Zhou, 2013: Using data to attribute episodes of warming and cooling in instrumental records. Proc. Natl. Acad. Sci. U.S.A., 110, 2058-2063. Turner, J., et al., 2005: Antarctic climate change during the last 50 years. Int. J. Climatol., 25, 279–294. Ulbrich, U., G. C. Leckebusch, and J. G. Pinto, 2009: Extra-tropical cyclones in the present and future climate: A review. Theor. Appl. Climatol., 96, 117–131. Uppala, S. M., et al., 2005: The ERA-40 re-analysis. Q. J. R. Meteorol. Soc., 131, 2961–3012. Usbeck, T., T. Wohlgemuth, C. Pfister, R. Volz, M. Beniston, and M. Dobbertin, 2010: Wind speed measurements and forest damage in Canton Zurich (Central Europe) from 1891 to winter 2007. Int. J. Climatol., 30, 347–358. Utsumi, N., S. Seto, S. Kanae, E. Maeda, and T. Oki, 2011: Does higher surface temperature intensify extreme precipitation? Geophys. Res. Lett., 38, L16708. van den Besselaar, E. J. M., A. M. G. Klein Tank, and T. A. Buishand, 2012: Trends in European precipitation extremes over 1951–2010. Int. J. Climatol., 33, 2682– 2689. van der Schrier, G., A. van Ulden, and G. J. van Oldenborgh, 2011: The construction of a Central Netherlands temperature. Clim. Past, 7, 527–542. van der Schrier, G., J. Barichivich, K. R. Briffa, and P. D. Jones, 2013: A scPDSI-based global dataset of dry and wet spells for 1901–2009. J. Geophys. Res. Atmos., 118, 4025-4048. van Haren, R., G. J. van Oldenborgh, G. Lenderink, M. Collins, and W. Hazeleger, 2012: SST and circulation trend biases cause an underestimation of European precipitation trends. Clim. Dyn., 40, 1-20. van Heerwaarden, C. C., J. V. G. de Arellano, and A. J. Teuling, 2010: Land-atmosphere coupling explains the link between pan evaporation and actual evapotranspiration trends in a changing climate. Geophys. Res. Lett., 37, L21401. van Ommen, T. D., and V. Morgan, 2010: Snowfall increase in coastal East Antarctica linked with southwest Western Australian drought. Nature Geosci., 3, 267–272. Vautard, R., P. Yiou, and G. J. van Oldenborgh, 2009: Decline of fog, mist and haze in Europe over the past 30 years. Nature Geosci., 2, 115–119. Vautard, R., J. Cattiaux, P. Yiou, J. N. The paut, and P. Ciais, 2010: Northern Hemisphere atmospheric stilling partly attributed to an increase in surface roughness. Nature Geosci., 3, 756-761. Vautard, R., et al., 2007: Summertime European heat and drought waves induced by wintertime Mediterranean rainfall deficit. Geophys. Res. Lett., 34., L07711 Vecchi, G. A., and B. J. Soden, 2007: Global warming and the weakening of the tropical circulation. J. Clim., 20, 4316–4340. Vecchi, G. A., and T. R. Knutson, 2008: On estimates of historical north Atlantic tropical cyclone activity. J. Clim., 21, 3580–3600. Vecchi, G. A., and T. R. Knutson, 2011: Estimating annual numbers of Atlantic hurricanes missing from the HURDAT database (1878–1965) using ship track density. J. Clim., 24, 1736–1746. Vecchi, G. A., B. J. Soden, A. T. Wittenberg, I. M. Held, A. Leetmaa, and M. J. Harrison, 2006: Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing. Nature, 441, 73–76. Velders, G., S. Andersen, J. Daniel, D. Fahey, and M. McFarland, 2007: The importance of the Montreal Protocol in protecting climate. Proc. Natl. Acad. Sci. U.S.A., 104, 4814-4819. Velders, G., D. Fahey, J. Daniel, M. McFarland, and S. Andersen, 2009: The large contribution of projected HFC emissions to future climate forcing. Proc. Natl. Acad. Sci. U.S.A., 106, 10949-10954. Venema, V. K. C., et al., 2012: Benchmarking homogenization algorithms for monthly data. Clim. Past, 8, 89–115. Verbout, S., H. Brooks, L. Leslie, and D. Schultz, 2006: Evolution of the US tornado database: 1954–2003. Weather Forecast., 21, 86–93. Vicente-Serrano, S. M., S. Begueria, and J. I. Lopez-Moreno, 2010: A multiscalar drought index sensitive to global warming: The Standardized Precipitation Evapotranspiration Index. J. Clim., 23, 1696–1718. Vidal, J., E. Martin, L. Franchisteguy, F. Habets, J. Soubeyroux, M. Blanchard, and M. Baillon, 2010: Multilevel and multiscale drought reanalysis over France with the Safran-Isba-Modcou hydrometeorological suite. Hydrol. Earth Syst. Sci., 14, 459–478. Vilibic, I., and J. Sepic, 2010: Long-term variability and trends of sea level storminess and extremes in European Seas. Global Planet. Change, 71, 1–12. Villarini, G., J. Smith, and G. Vecchi, 2013: Changing frequency of heavy rainfall over the central United States. J. Clim., 26, 351–357. Vincent, L., et al., 2011: Observed trends in indices of daily and extreme temperature and precipitation for the countries of the western Indian Ocean, 1961–2008. J. Geophys. Res. Atmos., 116, D10108. Vincent, L. A., X. L. L. Wang, E. J. Milewska, H. Wan, F. Yang, and V. Swail, 2012: A second generation of homogenized Canadian monthly surface air temperature for climate trend analysis. J. Geophys. Res. Atmos., 117, D18110. Visbeck, M., 2009: A station-based Southern Annular Mode Index from 1884 to 2005. J. Clim., 22, 940–950. Volz, A., and D. Kley, 1988: Evaluation of the Montsouris series of ozone measurements made in the 19th century. Nature, 332, 240–242. Vömel, H., D. E. David, and K. Smith, 2007a: Accuracy of tropospheric and stratospheric water vapor measurements by the cryogenic frost point hygrometer: Instrumental details and observations. J. Geophys. Res. Atmos., 112, D08305. Vömel, H., et al., 2007b: Validation of Aura Microwave Limb Sounder water vapor by balloon-borne cryogenic frost point hygrometer measurements. J. Geophys. Res. Atmos., 112, D24S37. von Clarmann, T., et al., 2009: Retrieval of temperature, H2O, O3, HNO3, CH4, N2O, ClONO2 and ClO from MIPAS reduced resolution nominal mode limb emission measurements. Atmos. Meas. Tech., 2, 159–175. von Schuckmann, K., and P.-Y. Le Traon, 2011: How well can we derive global ocean indicators from Argo data? Ocean Sci., 7, 783–791. Von Storch, H., 1999: Misuses of statistical analysis in climate research. Analysis of Climate Variability: Applications of Statistical Techniques, 2nd edition [H. Von Storch and A. Navarra (eds.)]. Springer-Verlag, New York, and Heidelberg, Germany, pp. 11–26. von Storch, H., and F. W. Zwiers, 1999: Statistical Analysis in Climate Research. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 484 pp. Vose, R. S., D. R. Easterling, and B. Gleason, 2005a: Maximum and minimum temperature trends for the globe: An update through 2004. Geophys. Res. Lett., 32, L23822. Vose, R. S., D. Wuertz, T. C. Peterson, and P. D. Jones, 2005b: An intercomparison of trends in surface air temperature analyses at the global, hemispheric, and gridbox scale. Geophys. Res. Lett., 32, L18718. Vose, R. S., S. Applequist, M. J. Menne, C. N. Williams, Jr., and P. Thorne, 2012a: An intercomparison of temperature trends in the US Historical Climatology Network and recent atmospheric reanalyses. Geophys. Res. Lett., 39, L10703. Vose, R. S., Oak Ridge National Laboratory. Environmental Sciences Division., U.S. Global Change Research Program, United States. Dept. of Energy. Office of Health and Environmental Research., Carbon Dioxide Information Analysis Center (U.S.), and Martin Marietta Energy Systems Inc., 1992: The Global Historical Climatology Network: Long-Term Monthly Temperature, Precipitation, Sea Level Pressure, and Station Pressure Data. Carbon Dioxide Information Analysis Center. Available to the public from N.T.I.S., 1 v. (various pagings) Vose, R. S., et al., 2012b: NOAA’s Merged Land-Ocean Surface Temperature Analysis. Bull. Am. Meteor. Soc., 93, 1677–1685. Wacker, S., J. Grobner, K. Hocke, N. Kampfer, and L. Vuilleumier, 2011: Trend analysis of surface cloud-free downwelling long-wave radiation from four Swiss sites. J. Geophys. Res. Atmos., 116, 13. Wallace, J. M., and D. S. Gutzler, 1981: Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon. Weather Rev., 109, 784–812. Wan, H., X. L. Wang, and V. R. Swail, 2010: Homogenization and trend analysis of Canadian near-surface wind speeds. J. Clim., 23, 1209–1225. Wan, H., X. Zhang, F. Zwiers, S. Emori, and H. Shiogama, 2013: Effect of data coverage on the estimation of mean and variability of precipitation at global and regional scales. J. Geophys. Res., 118, 534–546. Wang, B., J. Liu, H. J. Kim, P. J. Webster, and S. Y. Yim, 2012a: Recent change of the global monsoon precipitation (1979–2008). Clim. Dyn., 39, 1123–1135. Wang, H., et al., 2012b: Extreme climate in China: Facts, simulation and projection. Meteorol. Z., 21, 279–304. Wang, J. H., and L. Y. Zhang, 2008: Systematic errors in global radiosonde precipitable water data from comparisons with ground-based GPS measurements. J. Clim., 21, 2218–2238. Wang, J. H., and L. Y. Zhang, 2009: Climate applications of a global, 2-hourly atmospheric precipitable water dataset derived from IGS tropospheric products. J. Geodes., 83, 209–217. Wang, J. H., L. Y. Zhang, A. Dai, T. Van Hove, and J. Van Baelen, 2007: A near-global, 2-hourly data set of atmospheric precipitable water from ground-based GPS measurements. J. Geophys. Res. Atmos., 112, D11107. Wang, J. S., D. J. Seidel, and M. Free, 2012c: How well do we know recent climate trends at the tropical tropopause? J. Geophys. Res. Atmos., 117, D09118. Wang, K., R. E. Dickinson, and S. Liang, 2009a: Clear sky visibility has decreased over land globally from 1973 to 2007. Science, 323, 1468–1470. Wang, K., H. Ye, F. Chen, Y. Z. Xiong, and C. P. Wang, 2012d: Urbanization effect on the diurnal temperature range: Different roles under solar dimming and brightening. J. Clim., 25, 1022–1027. Wang, K. C., and S. L. Liang, 2009: Global atmospheric downward longwave radiation over land surface under all-sky conditions from 1973 to 2008. J. Geophys. Res. Atmos., 114, D19101. Wang, K. C., R. E. Dickinson, and S. L. Liang, 2009b: Clear sky visibility has decreased over land globally from 1973 to 2007. Science, 323, 1468–1470. Wang, K. C., R. E. Dickinson, M. Wild, and S. L. Liang, 2010: Evidence for decadal variation in global terrestrial evapotranspiration between 1982 and 2002: 2. Results. J. Geophys. Res. Atmos., 115, D20113. Wang, K. C., R. E. Dickinson, M. Wild, and S. Liang, 2012e: Atmospheric impacts on climatic variability of surface incident solar radiation. Atmos. Chem. Phys., 12, 9581–9592. Wang, K. C., R. E. Dickinson, L. Su, and K. E. Trenberth, 2012f: Contrasting trends of mass and optical properties of aerosols over the Northern Hemisphere from 1992 to 2011. Atmos. Chem. Phys., 12, 9387–9398. Wang, L. K., C. Z. Zou, and H. F. Qian, 2012g: Construction of stratospheric temperature data records from Stratospheric Sounding Units. J. Clim., 25, 2931–2946. Wang, X., H. Wan, and V. Swail, 2006a: Observed changes in cyclone activity in Canada and their relationships to major circulation regimes. J. Clim., 19, 896– 915. Wang, X., B. Trewin, Y. Feng, and D. Jones, 2013: Historical changes in Australian temperature extremes as inferred from extreme value distribution analysis. Geophys. Res. Lett., 40, 573-578. Wang, X., Y. Feng, G. P. Compo, V. R. Swail, F. W. Zwiers, R. J. Allan, and P. D. Sardeshmukh, 2012: Trends and low frequency variability of extra-tropical cyclone activity in the ensemble of twentieth century reanalysis. Clim. Dyn., 40, 2775-2800. Wang, X., et al., 2011: Trends and low-frequency variability of storminess over western Europe, 1878–2007. Clim. Dyn., 37, 2355-2371. Wang, X. L. L., V. R. Swail, and F. W. Zwiers, 2006b: Climatology and changes of extratropical cyclone activity: Comparison of ERA-40 with NCEP-NCAR reanalysis for 1958–2001. J. Clim., 19, 3145–3166. Wang, X. L. L., F. W. Zwiers, V. R. Swail, and Y. Feng, 2009c: Trends and variability of storminess in the Northeast Atlantic region, 1874–2007. Clim. Dyn., 33, 1179–1195. Wang, X. M., P. M. Zhai, and C. C. Wang, 2009d: Variations in extratropical cyclone activity in northern East Asia. Adv. Atmos. Sci., 26, 471–479. Warren, S. G., R. M. Eastman, and C. J. Hahn, 2007: A survey of changes in cloud cover and cloud types over land from surface observations, 1971–96. J. Clim., 20, 717–738. Weaver, S. J., 2012: Factors associated with decadal variability in Great Plains summertime surface temperatures. J. Clim., 26, 343–350. Weber, M., W. Steinbrecht, C. Long, V. E. Fioletov, S. H. Frith, R. Stolarski, and P. A. Newman, 2012: Stratospheric ozone [in “State of the Climate in 2011”]. Bull. Am. Met. Soc., 93, S46–S44. Weinkle, J., R. Maue, and R. Pielke, 2012: Historical global tropical cyclone landfalls. J. Clim., 25, 4729–4735. Weinstock, E. M., et al., 2009: Validation of the Harvard Lyman-alpha in situ water vapor instrument: Implications for the mechanisms that control stratospheric water vapor. J. Geophys. Res. Atmos., 114. Weiss, R., J. Muhle, P. Salameh, and C. Harth, 2008: Nitrogen trifluoride in the global atmosphere. Geophys. Res. Lett., 35, L20821. Wells, N., S. Goddard, and M. J. Hayes, 2004: A self-calibrating Palmer Drought Severity Index. J. Clim., 17, 2335–2351. Wentz, F., C. Gentemann, D. Smith, and D. Chelton, 2000: Satellite measurements of sea surface temperature through clouds. Science, 288, 847–850. Wentz, F. J., L. Ricciardulli, K. Hilburn, and C. Mears, 2007: How much more rain will global warming bring? Science, 317, 233–235. Werner, P. C., F. W. Gerstengarbe, and F. Wechsung, 2008: Grosswetterlagen and precipitation trends in the Elbe River catchment. Meteorol. Z., 17, 61–66. Westra, S., and S. Sisson, 2011: Detection of non-stationarity in precipitation extremes using a max-stable process model. J. Hydrol., 406, 119–128. Westra, S., L. Alexander, and F. Zwiers, 2013: Global increasing trends in annual maximum daily precipitation. J. Clim., 26, 3904-3918. Wibig, J., 2008: Cloudiness variations in Lodz in the second half of the 20th century. Int. J. Climatol., 28, 479–491. Wickham, C., et al., 2013: Influence of urban heating on the global temperature land average using rural sites identified from MODIS classifications. Geoinfor Geostat: An Overview, 1, 1:2. doi:10.4172/gigs.1000104. Wielicki, B. A., B. R. Barkstrom, E. F. Harrison, R. B. Lee, G. L. Smith, and J. E. Cooper, 1996: Clouds and the Earth’s radiant energy system (CERES): An Earth observing system experiment. Bull. Am. Meteor. Soc., 77, 853–868. Wielicki, B. A., et al., 2002: Evidence for large decadal variability in the tropical mean radiative energy budget. Science, 295, 841–844. Wilby, R. L., P. D. Jones, and D. H. Lister, 2011: Decadal variations in the nocturnal heat island of London. Weather, 66, 59–64. Wild, M., 2009: Global dimming and brightening: A review. J. Geophys. Res. Atmos., 114, D00D16. Wild, M., 2012: Enlightening global dimming and brightening. Bull. Am. Meteor. Soc., 93, 27–37. Wild, M., A. Ohmura, and K. Makowski, 2007: Impact of global dimming and brightening on global warming. Geophys. Res. Lett., 34, L04702. Wild, M., J. Grieser, and C. Schaer, 2008: Combined surface solar brightening and increasing greenhouse effect support recent intensification of the global landbased hydrological cycle. Geophys. Res. Lett., 35, L17706. Wild, M., A. Ohmura, H. Gilgen, and D. Rosenfeld, 2004: On the consistency of trends in radiation and temperature records and implications for the global hydrological cycle. Geophys. Res. Lett., 31, L11201. Wild, M., A. Ohmura, H. Gilgen, E. Roeckner, M. Giorgetta, and J. J. Morcrette, 1998: The disposition of radiative energy in the global climate system: GCM-calculated versus observational estimates. Clim. Dyn., 14, 853–869. Wild, M., D. Folini, C. Schär, N. Loeb, E. G. Dutton, and G. König-Langlo, 2013: The global energy balance from a surface perspective. Clim. Dyn., 40, 3107-3134. Wild, M., B. Truessel, A. Ohmura, C. N. Long, G. Konig-Langlo, E. G. Dutton, and A. Tsvetkov, 2009: Global dimming and brightening: An update beyond 2000. J. Geophys. Res. Atmos., 114, D00d13. Wild, M., et al., 2005: From dimming to brightening: Decadal changes in solar radiation at Earth’s surface. Science, 308, 847–850. Wilks, D. S., 2006: Statistical Methods in the Atmospheric Sciences, 2nd edition. Elsevier, Philadelphia, 627 pp. Willett, K. M., P. D. Jones, N. P. Gillett, and P. W. Thorne, 2008: Recent Changes in Surface Humidity: Development of the HadCRUH dataset. J. Clim., 21, 5364–5383. Willett, K. M., P. D. Jones, P. W. Thorne, and N. P. Gillett, 2010: A comparison of large scale changes in surface humidity over land in observations and CMIP3 general circulation models. Environ. Res. Lett., 5. Willett, K. M., et al., 2013: HadISDH: an updateable land surface specific humidity product for climate monitoring. Clim. Past, 9, 657–677. Williams, C. N., M. J. Menne, and P. W. Thorne, 2012: Benchmarking the performance of pairwise homogenization of surface temperatures in the United States. J. Geophys. Res. Atmos., 117. Willson, R. C., and A. V. Mordvinov, 2003: Secular total solar irradiance trend during solar cycles 21–23. Geophys. Res. Lett., 30, 1199. Winkler, P., 2009: Revision and necessary correction of the long-term temperature series of Hohenpeissenberg, 1781–2006. Theor. Appl. Climatol., 98, 259–268. Wong, T., B. A. Wielicki, R. B. Lee, ., G. L. Smith, K. A. Bush, and J. K. Willis, 2006: Reexamination of the observed decadal variability of the earth radiation budget using altitude-corrected ERBE/ERBS nonscanner WFOV data. J. Clim., 19, 4028–4040. Wood, S. N., 2006: Generalized Additive Models: An Introduction with R. CRC/Chapman & Hall, Boca Raton, FL, USA. Woodruff, S. D., et al., 2011: ICOADS Release 2.5: Extensions and enhancements to the Surface Marine Meteorological Archive. Int. J. Climatol., 31, 951–967. Worden, H. M., et al., 2013: Decadal record of satellite carbon monoxide observations. Atmos. Chem. Phys., 13, 837–850. Worton, D., et al., 2007: Atmospheric trends and radiative forcings of CF4 and C2F6 inferred from firn air. Environ. Sci. Technol., 41, 2184-2189. Worton, D. R., et al., 2012: Evidence from firn air for recent decreases in non-methane hydrocarbons and a 20th century increase in nitrogen oxides in the northern hemisphere. Atmos. Environ., 54, 592–602. Wu, Z., N. E. Huang, S. R. Long, and C.-K. Peng, 2007: On the trend, detrending, and variability of nonlinear and nonstationary time series. Proc. Natl. Acad. Sci. U.S.A., 104, 14889–14894. Wu, Z., N. E. Huang, J. M. Wallace, B. V. Smoliak, and X. Chen, 2011: On the timevarying trend in global-mean surface temperature. Clim. Dyn., 37, 759–773. Xavier, P. K., V. O. John, S. A. Buehler, R. S. Ajayamohan, and S. Sijikumar, 2010: Variability of Indian summer monsoon in a new upper tropospheric humidity data set. Geophys. Res. Lett., 37, L05705. Xia, X., 2010a: A closer looking at dimming and brightening in China during 1961– 2005. Ann. Geophys., 28, 1121–1132. Xia, X. G., 2010b: Spatiotemporal changes in sunshine duration and cloud amount as well as their relationship in China during 1954–2005. J. Geophys. Res. Atmos., 115, D00K06. Xiao, X., et al., 2010: Atmospheric three-dimensional inverse modeling of regional industrial emissions and global oceanic uptake of carbon tetrachloride. Atmos. Chem. Phys., 10, 10421–10434. Xie, B., Q. Zhang, and Y. Wang, 2010: Observed characteristics of hail size in four regions in China during 1980–2005. J. Clim., 23, 4973–4982. Xie, B. G., Q. H. Zhang, and Y. Q. Wang, 2008: Trends in hail in China during 1960– 2005. Geophys. Res. Lett., 35, L13801. Xie, S., K. Hu, J. Hafner, H. Tokinaga, Y. Du, G. Huang, and T. Sampe, 2009: Indian Ocean capacitor effect on Indo-Western Pacific climate during the summer following El Niño. J. Clim., 22, 730–747. Xu, C. Y., L. B. Gong, J. Tong, and D. L. Chen, 2006a: Decreasing reference evapotranspiration in a warming climate – A case of Changjiang (Yangtze) River catchment during 1970–2000. Adv. Atmos. Sci., 23, 513–520. Xu, K. H., J. D. Milliman, and H. Xu, 2010: Temporal trend of precipitation and runoff in major Chinese Rivers since 1951. Global Planet. Change, 73, 219–232. Xu, M., C. P. Chang, C. B. Fu, Y. Qi, A. Robock, D. Robinson, and H. M. Zhang, 2006b: Steady decline of east Asian monsoon winds, 1969–2000: Evidence from direct ground measurements of wind speed. J. Geophys. Res. Atmos., 111. Yan, Z. W., Z. Li, Q. X. Li, and P. Jones, 2010: Effects of site change and urbanisation in the Beijing temperature series 1977–2006. Int. J. Climatol., 30, 1226–1234. Yang, J., Q. Liu, S.-P. Xie, Z. Liu, and L. Wu, 2007: Impact of the Indian Ocean SST basin mode on the Asian summer monsoon. Geophys. Res. Lett., 34, L02708. Yang, X. C., Y. L. Hou, and B. D. Chen, 2011: Observed surface warming induced by urbanization in east China. J. Geophys. Res. Atmos., 116, 12. Yokouchi, Y., S. Taguchi, T. Saito, Y. Tohjima, H. Tanimoto, and H. Mukai, 2006: High frequency measurements of HFCs at a remote site in east Asia and their implications for Chinese emissions. Geophys. Res. Lett., 33, L21814. Yoon, J., W. von Hoyningen-Huene, A. A. Kokhanovsky, M. Vountas, and J. P. Burrows, 2012: Trend analysis of aerosol optical thickness and Angstrom exponent derived from the global AERONET spectral observations. Atmos. Meas. Tech., 5, 1271–1299. You, Q., et al., 2010: Changes in daily climate extremes in China and their connection to the large scale atmospheric circulation during 1961–2003. Clim. Dyn., 36, 2399-2417. Yttri, K. E., et al., 2011: Transboundary particulate matter in Europe, Status Report 2011. In: Co-operative Programme for Monitoring and Evaluation of the Long Range Transmission of Air Pollutants (Joint CCC, MSC-W, CEIP and CIAM report 2011). NILU - Chemical Coordinating Centre - CCC. Blank page common_publications.html Yu, B., and F. W. Zwiers, 2010: Changes in equatorial atmospheric zonal circulations in recent decades. Geophys. Res. Lett., 37, L05701. Yu, L., and R. Weller, 2007: Objectively analyzed air-sea heat fluxes for the global ice-free oceans (1981–2005). Bull. Am. Meteor. Soc., 88, 527-539. Yuan, X., and C. Li, 2008: Climate modes in southern high latitudes and their impacts on Antarctic sea ice. J. Geophys. Res. Oceans, 113, C06S91. Yurganov, L., W. McMillan, E. Grechko, and A. Dzhola, 2010: Analysis of global and regional CO burdens measured from space between 2000 and 2009 and validated by ground-based solar tracking spectrometers. Atmos. Chem. Phys., 10, 3479–3494. Zebiak, S. E., 1993: Air-sea interaction in the equatorial Atlantic region. J. Clim., 6, 1567–1568. Zerefos, C. S., et al., 2009: Solar dimming and brightening over Thessaloniki, Greece, and Beijing, China. Tellus B, 61, 657–665. Zhang, A. Y., G. Y. Ren, J. X. Zhou, Z. Y. Chu, Y. Y. Ren, and G. L. Tang, 2010: On the urbanization effect on surface air temperature trends over China. Acta Meteorol. Sin., 68, 957–966. Zhang, H., J. Bates, and R. Reynolds, 2006: Assessment of composite global sampling: Sea srface wind speed. Geophys. Res. Lett., 33, L17714. Zhang, J., and J. S. Reid, 2010: A decadal regional and global trend analysis of the aerosol optical depth using a data-assimilation grade over-water MODIS and Level 2 MISR aerosol products. Atmos. Chem. Phys., 10, 10949–10963. Zhang, X., J. He, J. Zhang, I. Polaykov, R. Gerdes, J. Inoue, and P. Wu, 2012a: Enhanced poleward moisture transport and amplified northern high-latitude wetting trend. Nature Clim. Change, 3, 47-51. Zhang, X., et al., 2007a: Detection of human influence on twentieth-century precipitation trends. Nature, 448, 461–U464. Zhang, X., et al., 2011: Indices for monitoring changes in extremes based on daily temperature and precipitation data. Wiley Interdis. Rev. Clim. Change, 2, 851- 870. Zhang, X. B., et al., 2005: Trends in Middle East climate extreme indices from 1950 to 2003. J. Geophys. Res. Atmos., 110, D22104. Zhang, X. D., C. H. Lu, and Z. Y. Guan, 2012b: Weakened cyclones, intensified anticyclones and recent extreme cold winter weather events in Eurasia. Environ. Res. Lett., 7, 044044. Zhang, X. D., J. E. Walsh, J. Zhang, U. S. Bhatt, and M. Ikeda, 2004: Climatology and interannual variability of Arctic cyclone activity: 1948–2002. J. Clim., 17, 2300–2317. Zhang, Y., J. M. Wallace, and D. S. Battisti, 1997: ENSO-like interdecadal variability: 1900–93. J. Clim., 10, 1004–1020. Zhang, Y. Q., C. M. Liu, Y. H. Tang, and Y. H. Yang, 2007b: Trends in pan evaporation and reference and actual evapotranspiration across the Tibetan Plateau. J. Geophys. Res. Atmos., 112, D12110. Zhao, X. P. T., A. K. Heidinger, and K. R. Knapp, 2011: Long-term trends of zonally averaged aerosol optical thickness observed from operational satellite AVHRR instrument. Meteorol. Appl., 18, 440–445. Zhen, L., and Y. Zhong-Wei, 2009: Homogenized daily mean.maximum/minimum temperature series for China from 1960–2008. 237–243. Zhou, J., and K.-K. Tung, 2012: Deducing multidecadal anthropogenic global warming trends using multiple regression Analysis. J. Atmos. Sci., 70, 3–8. Zhou, T., L. Zhang, and H. Li, 2008: Changes in global land monsoon area and total rainfall accumulation over the last half century. Geophys. Res. Lett., 35, L16707. Zhou, T. J., D. Y. Gong, J. Li, and B. Li, 2009a: Detecting and understanding the multidecadal variability of the East Asian summer monsoon – Recent progress and state of affairs. Meteorol. Z., 18, 455–467. Zhou, T. J., et al., 2009b: Why the Western Pacific subtropical high has extended westward since the late 1970s. J. Clim., 22, 2199–2215. Zhou, Y. P., K. M. Xu, Y. C. Sud, and A. K. Betts, 2011: Recent trends of the tropical hydrological cycle inferred from Global Precipitation Climatology Project and International Satellite Cloud Climatology Project data. J. Geophys. Res. Atmos., 116, D09101 Zhou, Y. Q., and G. Y. Ren, 2011: Change in extreme temperature event frequency over mainland China, 1961–2008. Clim. Res., 50, 125–139. Ziemke, J. R., S. Chandra, and P. K. Bhartia, 2005: A 25-year data record of atmospheric ozone in the Pacific from Total Ozone Mapping Spectrometer (TOMS) cloud slicing: Implications for ozone trends in the stratosphere and troposphere. J. Geophys. Res., 110, D15105. Ziemke, J. R., S. Chandra, G. J. Labow, P. K. Bhartia, L. Froidevaux, and J. C. Witte, 2011: A global climatology of tropospheric and stratospheric ozone derived from Aura OMI and MLS measurements. Atmos. Chem. Phys., 11, 9237–9251. Zipser, E. J., C. Liu, D. J. Cecil, S. W. Nesbitt, and D. P. Yorty, 2006: Where are the most intense thunderstorms on Earth? Bull. Am. Meteor. Soc., 87, 1057–1071. Zolina, O., C. Simmer, K. Belyaev, A. Kapala, and S. Gulev, 2009: Improving estimates of heavy and extreme precipitation using daily records from European rain gauges. J. Hydrometeor., 10, 701–716. Zorita, E., T. F. Stocker, and H. von Storch, 2008: How unusual is the recent series of warm years? Geophys. Res. Lett., 35, L24706. Zou, C. Z., and W. H. Wang, 2010: Stability of the MSU-derived atmospheric temperature trend. J. Atmos. Ocean Technol., 27, 1960–1971. Zou, C. Z., and W. H. Wang, 2011: Intersatellite calibration of AMSU-A observations for weather and climate applications. J. Geophys. Res. Atmos., 116, D23113. Zou, C. Z., M. D. Goldberg, Z. H. Cheng, N. C. Grody, J. T. Sullivan, C. Y. Cao, and D. Tarpley, 2006a: Recalibration of microwave sounding unit for climate studies using simultaneous nadir overpasses. J. Geophys. Res. Atmos., 111, L17701. Zou, X., L. V. Alexander, D. Parker, and J. Caesar, 2006b: Variations in severe storms over China. Geophys. Res. Lett., 33. Zwiers, F. W., and V. V. Kharin, 1998: Changes in the extremes of the climate simulated by CCC GCM2 under CO2 doubling. J. Clim., 11, 2200–2222.
 
FOOTNOTES REGARDING PROBABILITIES

1) In this Report, the following terms have been used to indicate the assessed likelihood of an outcome or a result: Virtually certain 99–100% probability, Very likely 90–100%, Likely 66–100%, About as likely as not 33–66%, Unlikely 0–33%, Very unlikely 0-10%, Exceptionally unlikely 0–1%. Additional terms (Extremely likely: 95–100%, More likely than not >50–100%, and Extremely unlikely 0–5%) may also be used when appropriate. Assessed likelihood is typeset in italics, e.g., very likely (see Section 1.4 and Box TS.1 for more details).

2) In this Report, the following summary terms are used to describe the available evidence: limited, medium, or robust; and for the degree of agreement: low, medium, or high. A level of confidence is expressed using five qualifiers: very low, low, medium, high, and very high, and typeset in italics, e.g., medium confidence. For a given evidence and agreement statement, different confidence levels can be assigned, but increasing levels of evidence and degrees of agreement are correlated with increasing confidence (see Section 1.4 and Box TS.1 for more details).
 
Al-Gore-Explains-Cold-Weather-701167.jpg
 
Are you under the impression that a change in the Earth's temperature of, say, 1C would cause all temperatures all over the planet, throughout the year, to rise? That any temperature anywhere going down PROVES that global warming is not taking place?

If so, you're a fucking idiot.
 
FOOTNOTES REGARDING PROBABILITIES

1) In this Report, the following terms have been used to indicate the assessed likelihood of an outcome or a result: Virtually certain 99–100% probability, Very likely 90–100%, Likely 66–100%, About as likely as not 33–66%, Unlikely 0–33%, Very unlikely 0-10%, Exceptionally unlikely 0–1%. Additional terms (Extremely likely: 95–100%, More likely than not >50–100%, and Extremely unlikely 0–5%) may also be used when appropriate. Assessed likelihood is typeset in italics, e.g., very likely (see Section 1.4 and Box TS.1 for more details).

2) In this Report, the following summary terms are used to describe the available evidence: limited, medium, or robust; and for the degree of agreement: low, medium, or high. A level of confidence is expressed using five qualifiers: very low, low, medium, high, and very high, and typeset in italics, e.g., medium confidence. For a given evidence and agreement statement, different confidence levels can be assigned, but increasing levels of evidence and degrees of agreement are correlated with increasing confidence (see Section 1.4 and Box TS.1 for more details).

Like I have been saying...no observed, measured evidence that supports AGW over natural variability....no observed, measured evidence that establishes a coherent link between the absorption of IR by a gas and warming in the atmosphere and no published, peer reviewed paper where the hypothesized warming due to mankind's burins of hydrocarbon fuels, which is the foundation of the anthropogenic global warming hypothesis has never been empirically measured, quantified, and then attributed to so called green house gasses.

Care to point out any of those in the steaming pile you brought forward? Didn't think so.

It is, as always, good to see what passes for actual evidence in that weak little mind of yours...it serves to illustrate how you were duped so easily.
 
It is, as always, disappointing to see you continue to lie to our faces.
 
It is, as always, disappointing to see you continue to lie to our faces.


Speaking of bald faced liars...you posted that big steaming pile of excrement claiming that it contained published, observed, empirical evidence of AGW...I read it and pointed out that it wasn't there, with the caveat that I might have missed something and asked you to point out where such evidence was...or observed evidence that supported AGW over natural variability, or observed evidence that supported a coherent link between the absorption of IR by a gas, and warming in the atmosphere...

I can't help but note that you can't do it even when the steaming pile is right there in front of your face...You have either been lying all this time about the evidence being in the IPCC paper, or you are so stupid that you don't have any idea what actual observed, measured evidence supporting one hypothesis over another looks like, or you are so dim and your bar for evidence is so low, that you think it is actually in there.

In any case, you claimed it was there, you posted it here and you have yet to point out anything there that even begins to answer my request...laughing in your face skidmark...

Whats the matter skidmark...cant bear to admit that it isn't there and never was?
 
Asshole, have you nothing of substance to contribute to the debate? Thus far, all you have been is a brainless troll, worth no respect at all. The science is settled. The absorption spectra of the GHG's was first measured one hundred and sixty years ago. The prediction of Arrhenious, made in 1896, are being borne out. The predictions of Dr. James Hansen, made in the 1980's, are spot on, and, if anything, are a bit conservative.

 
It is, as always, disappointing to see you continue to lie to our faces.


Speaking of bald faced liars...you posted that big steaming pile of excrement claiming that it contained published, observed, empirical evidence of AGW...I read it and pointed out that it wasn't there, with the caveat that I might have missed something and asked you to point out where such evidence was...or observed evidence that supported AGW over natural variability, or observed evidence that supported a coherent link between the absorption of IR by a gas, and warming in the atmosphere...

I can't help but note that you can't do it even when the steaming pile is right there in front of your face...You have either been lying all this time about the evidence being in the IPCC paper, or you are so stupid that you don't have any idea what actual observed, measured evidence supporting one hypothesis over another looks like, or you are so dim and your bar for evidence is so low, that you think it is actually in there.

In any case, you claimed it was there, you posted it here and you have yet to point out anything there that even begins to answer my request...laughing in your face skidmark...

Whats the matter skidmark...cant bear to admit that it isn't there and never was?

Did you fail to note the references I posted? No, you saw them. You just don't want to talk about them. I've never met anyone in my entire life that lies as much or as easily as do you. I think you actually lie more than Trump.
 
Did you fail to note the references I posted? No, you saw them. You just don't want to talk about them. I've never met anyone in my entire life that lies as much or as easily as do you. I think you actually lie more than Trump.

Yes...I saw them...and noted that you didn't point out anything there either...just reverences which were used to produce the steaming pile you posted which had not one shred of the sort of evidence I asked for, which you had been claiming for years was there...

You lied skidmark...you lied over and over and over for years and years...it isn't there...and it never was.
 

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