Since when did hot water sink?
When it's pushed against a coastline by sustained winds. Do you have some other explanation for this
Hot water always rises to the surface. And if you've ever gone swimming after a hurricane has passed you find the water is cold as hell from the wind generated waves bringing cold water to the surface. But it takes a hell of a lot of wind for that to happen.
I'm glad to see you've noted how moving warm water to the depths causes cold water to replace it at the surface. This process is responsible for a very large chunk of the reduction in surface warming witnessed since the turn of the millennium.
As to the validity of BTK 2013 - a large number of studies since BTK have come to virtually identical conclusions. They are accessible below.
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Papers that have cited BTK 2013
A statistical analysis of sea temperature data
Abstract
The paper analyzes sea temperature series measured at two geographical locations along the coast of Norway. We address the question whether the series are stable over the sample period 1936–2012 and whether we can measure any signal of climate change in the regional data. We use nonstandard supF, OLS-based CUSUM, RE, and Chow tests in combination with the Bai-Perron’s structural break test to identify potential changes in the temperature. The augmented Dickey-Fuller, the KPSS, and the nonparametric Phillips-Perron tests are in addition applied in the evaluation of the stochastic properties of the series. The analysis indicates that both series undergo similar structural instabilities in the form of small shifts in the temperature level. The temperature at Lista (58° 06′ N, 06° 38′ E) shifts downward about 1962 while the Skrova series (68° 12′ N, 14° 10′ E) shifts to a lower level about 1977. Both series shift upward about 1987, and after a period of increasing temperature, both series start leveling off about the turn of the millennium. The series have no significant stochastic or deterministic trend. The analysis indicates that the mean temperature has moved upward in decadal, small steps since the 1980s. The result is in accordance with recent analyses of sea temperatures in the North Atlantic. The findings are also related to the so-called hiatus phenomenon where natural variation in climate can mask global warming processes. The paper contributes to the discussion of applying objective methods in measuring climate change.
Atmospheric science: Increasing wind sinks heat
Nature Climate Change
172–173
(2014)
26 February 2014
Abstract
Surface global warming has stalled since around 2000 despite increasing atmospheric CO2. A study finds that recent strengthening of Pacific trade winds has enhanced heat transport from the surface to ocean depths, explaining most of the slowed surface warming.
Attributing the increase in Northern Hemisphere hot summers since the late 20th century
Article first published online: 25 JUL 2014
DOI: 10.1002/2014GL061062
©2014.
Geophysical Research Letters
Volume 41, Issue 14, pages 5192–5199, 28 July 2014
Abstract
Anomalously high summertime temperatures have occurred with increasing frequency since the late 20th century. It is not clear why hot summers are becoming more frequent despite the recent slowdown in the rise in global surface air temperature. To examine factors affecting the historical variation in the frequency of hot summers over the Northern Hemisphere (NH), we conducted three sets of ensemble simulations with an atmospheric general circulation model. The model accurately reproduced interannual variation and long-term increase in the occurrence of hot summers. Decadal variabilities in the Pacific and Atlantic Oceans accounted for 43 ± 27% of the recent increase over the NH middle latitudes. In addition, direct influence of anthropogenic forcing also contributes to increasing the frequency since the late 20th century. The results suggest that the heat extremes can become more frequent in the coming decade even with the persistent slowdown in the global-mean surface warming.
Ocean Dynamics
June 2014, Volume 64,
Issue 6, pp 823-832
Date: 04 May 2014
Basin patterns of upper ocean warming for 1993–2009
Abstract
A previous study (Lyman et al., Nature 465:334–337, 2010) showed a robust warming signal of the global upper ocean (0–700 m). They examined several sources of uncertainty that contribute to differences among heat content estimations. However, their focus was limited to globally averaged estimation. This study presents the spatial pattern of the global heat content change based on observed gridded datasets (Levitus et al., Geophys Res Lett 36:L07608, 2009). The western Pacific, Atlantic, and Indian Oceans showed significant warming trends, whereas eastern Pacific and some areas of the Gulf Stream experienced negative trends during 1993–2009. Steady warming trend was obtained from the first EOF mode when El Nino and Southern Oscillation (ENSO)-related signals were removed. This result implies that the rapid increase in heat content of the upper ocean around 2000–2005 is not related to a sampling transition from XBT to Argo observations but is associated with a natural variability dominated by strong ENSO-related signals.
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Victor Klemas, Xiao-Hai Yan, Subsurface and deeper ocean remote sensing from satellites: An overview and new results,Progress in Oceanography, 2014, 122, 1
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Patrick T. Brown, Wenhong Li, Laifang Li, Yi Ming, Top-of-atmosphere radiative contribution to unforced decadal global temperature variability in climate models, Geophysical Research Letters, 2014, 41, 14
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H Annamalai, Climate Change and Water Resources, 2014,
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K.E. Trenberth, Reference Module in Earth Systems and Environmental Sciences, 2014,
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Henk-Jan T. Hoving, Jose Angel A. Perez, Kathrin S.R. Bolstad, Heather E. Braid, Aaron B. Evans, Dirk Fuchs, Heather Judkins, Jesse T. Kelly, José E.A.R. Marian, Ryuta Nakajima, Uwe Piatkowski, Amanda Reid, Michael Vecchione, José C.C. Xavier, Advances in Cephalopod Science: Biology, Ecology, Cultivation and Fisheries, 2014,
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Kevin E. Trenberth, John T. Fasullo, An apparent hiatus in global warming?, Earth's Future, 2013, 1, 1
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T. Wheeler, J. von Braun, Climate Change Impacts on Global Food Security, Science, 2013, 341, 6145, 508
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Isaac M. Held, Climate science: The cause of the pause, Nature, 2013, 501, 7467, 318
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Gerald A. Meehl, Aixue Hu, Julie M. Arblaster, John Fasullo, Kevin E. Trenberth, Externally Forced and Internally Generated Decadal Climate Variability Associated with the Interdecadal Pacific Oscillation, Journal of Climate, 2013, 26, 18, 7298
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Tim Cowan, Wenju Cai, Ariaan Purich, Leon Rotstayn, Matthew H. England, Forcing of anthropogenic aerosols on temperature trends of the sub-thermocline southern Indian Ocean, Scientific Reports, 2013, 3,
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Kevin E. Trenberth, John T. Fasullo, Regional Energy and Water Cycles: Transports from Ocean to Land, Journal of Climate,2013, 26, 20, 7837
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Masahiro Watanabe, Youichi Kamae, Masakazu Yoshimori, Akira Oka, Makiko Sato, Masayoshi Ishii, Takashi Mochizuki,Masahide Kimoto, Strengthening of ocean heat uptake efficiency associated with the recent climate hiatus, Geophysical Research Letters, 2013, 40, 12
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