Climate Models Look Good When Predicting Climate Change
ScienceDaily (Apr. 6, 2008) — The accuracy of computer models that predict climate change over the coming decades has been the subject of debate among politicians, environmentalists and even scientists. A new study by meteorologists at the University of Utah shows that current climate models are quite accurate and can be valuable tools for those seeking solutions on reversing global warming trends. Most of these models project a global warming trend that amounts to about 7 degrees Fahrenheit over the next 100 years.
In the study, co-authors Thomas Reichler and Junsu Kim from the Department of Meteorology at the University of Utah investigate how well climate models actually do their job in simulating climate. To this end, they compare the output of the models against observations for present climate. The authors apply this method to about 50 different national and international models that were developed over the past two decades at major climate research centers in China, Russia, Australia, Canada, France, Korea, Great Britain, Germany, and the United States. Of course, also included is the very latest model generation that was used for the very recent (2007) report of the Intergovernmental Panel on Climate Change (IPCC).
"Coupled models are becoming increasingly reliable tools for understanding climate and climate change, and the best models are now capable of simulating present-day climate with accuracy approaching conventional atmospheric observations," said Reichler. "We can now place a much higher level of confidence in model-based projections of climate change than in the past."
The many hours of studying models and comparing them with actual climate changes fulfills the increasing wish to know how much one can trust climate models and their predictions. Given the significance of climate change research in public policy, the study's results also provide important response to critics of global warming. Earlier this year, working group one of the IPCC released its fourth global warming report. The University of Utah study results directly relate to this highly publicized report by showing that the models used for the IPCC paper have reached an unprecedented level of realism.
Climate Models Look Good When Predicting Climate Change
All of the models used to forecast climate with regard to global warming are substantially inaccurate and in any event are not sufficiently accurate to provide a basis for decision making.
It turns out that climate is so complex that it is beyond our current understanding, much less our ability to build accurate computer models. Dr. James Hansen, a prominent scientist and leading proponent of human contribution to global warming, summed up the accuracy issue by saying, “The forcings that drive long-term climate change are not known with an accuracy sufficient to define future climate change.”
And, climate may be chaotic and therefore unmodelable, even in theory.
Further, essentially no one disputes that this is the case. There is a "scientific consensus" that the models are inaccurate that is more comprehensive than the consensus that humans are contributing to global warming.
In October 2007 Gerard Roe of the University of Washington led a study published in Science that basically reiterates and validates these points.
"The authors call on policymakers to 'resist the temptation to fix a [CO2] concentration target early on. Once fixed, it may be politically impossible to reduce it.'
Mark Cane, a climate scientist at Columbia University in New York City, said, 'A lot of the rhetoric about climate change has said we shouldn't do anything [about it] because it's uncertain.'
But with this new study, he said, 'we now know that this uncertainty will not go away.'
Experts agree that they can still improve shorter-term predictions of climate change for the next several decades and better forecast how particular regions will fare."
We are left with three facts: the greenhouse effect is real, carbon dioxide emissions have increased exponentially since the Industrial Revolution and temperatures have risen about 6° C (1.1° F) during the past century. The rest is speculation, or what I call religion.
Human-driven climate change can amount to not much, be catastrophic, or anything in between, and we simply do not know.
Even more distressing is that there is no way to know if any particular target, such as a 90% reduction by 2050, or the Kyoto targets, will have their intended effects.
Politicians and scientists are essentially dealing with random numbers.
However, no one discusses model inaccuracy because doubt can lead to inaction. And those who follow the gospel according to Al insist that there be immediate action, so that doubt is not to be abided.
(I am in the, global warming is real, camp, however, I believe that facts are important when discussing such an important issue, and the fact is that the models we are using to base political decisions are not up to the task - period.)
From the New Scientist, May 3, 2008 (emphasis mine)
... In a paper in the April edition of the Bulletin of the American Meteorological Society he (Palmer) warns that models often share the same biases and blind spots about features of the climate system that are critical for regional forecasts. They cannot reproduce El Niños in the Pacific Ocean, for instance. Nor can they simulate the weather systems that bring drought to the Sahel region of Africa, or the Atlantic storm tracks and blocking high-pressure zones that determine whether western Europe is wet or dry.
Last year, a panel on climate modeling that was preparing the ground for next week's summit concluded that current models "have serious limitations" and that their uncertainties "compromise the goal of providing society with reliable predictions of regional climate change". the panel, chaired by Jagadish Shukla of George Mason University in Claverton, Maryland, dismissed many current regional predictions as "laughable".
But whatever the uncertainties at the local level, the big picture remains clear. Our planet is straying into unknown climatic territory, with consequences that we probably have to accept are almost impossible to predict. ...
From the Royal Society
Following are excepts from "Confidence, uncertainty and decision-support relevance in climate predictions" from the Philosophical Transactions of the Royal Society by Stainforth, et al. (remember to take into account that the paper is written in reserved, diplomatic terms):
The reality of anthropogenic climate change is well documented and widely accepted. The media and policy makers are calling out for predictions regarding expected changes to their local climate. Providing direct quantitative answers to these calls is perceived as important for engaging the public in the issue and therefore the task of mitigation. It is also often seen as critical for adaptation and decision making by businesses, governments and individuals. The extent to which these calls can be answered today is unclear, given the state of the science.
There is no compulsion to hold that the most comprehensive models available will yield decision-relevant probabilities, even if those models are based upon ‘fundamental physics’.
Statements about future climate relate to a never before experienced state of the system; thus, it is impossible to either calibrate the model for the forecast regime of interest or confirm the usefulness of the forecasting process. Development and improvement of long time-scale processes are therefore reliant solely on tests of internal consistency and physical understanding of the processes involved, guided by information on past climatic states deduced from proxy data.
The interpretation of climate models to inform policy and decision support must consider at least five distinct sources of uncertainty. Forcing uncertainty captures those things in the future which are considered outside the climate system per se, yet affect it. Initial condition uncertainty captures our uncertainty in how to initialize the models in hand; what initial state, or ensemble of states, to integrate forward in time. Initial condition uncertainty is usefully divided into two camps depending on whether or not the details of todayÂ’s uncertainty in a variable are likely to influence the final distributions we estimate on our time scale of interest. Model imperfection describes the uncertainty resulting from our limited understanding of, and ability to simulate, the EarthÂ’s climate. It is also usefully divided into two types: uncertainty and inadequacy. Model uncertainty captures the fact that we are uncertain as to what parameter values (or ensembles of parameter values) are likely to provide the most informative results; here, climate modelling (sic) has a further complication due to choices between parametrizations (sic) themselves, not just the values of each model parameter. Finally, model inadequacy captures the fact that we know a priori, there is no combination of parametrizations (sic), parameter values and ICs which would accurately mimic all relevant aspects of the climate system. We know that, if nothing else, computational constraints prevent our models from any claim of near isomorphism with reality, whatever that phrase might mean. The five types of uncertainty are not independent and basic questions of identifiability and interpretation remain (Smith 2000). The design and interpretation of experiments in the face of these uncertainties are among the grand challenges of climate science today.
For many sources of inadequacy,the nonlinearity of the model suggests that we are unable to speculate on even the sign of that impact.
The model simulations are therefore taken as possibilities for future real world climate and as such of potential value to society, at least on variables and scales where the models agree in terms of their climate distributions (Smith 2002). But even best available information may be rationally judged quantitatively irrelevant for decision-support applications.
First, we must acknowledge that there are many areas for model improvement. Examples are the inclusion of a stratosphere, a carbon cycle, atmospheric/oceanic chemistry at some degree of complexity, ice-sheet dynamics, and realistic (i.e. statistically plausible equivalents of real-world behaviour) ENSO structures, land surface schemes (critical for exploration of regional feedbacks), a grand ensemble-deduced transfer function diurnal cycles, hurricanes, ocean eddies and many others.
Models of such complexity, at high resolution and with suitable exploration of uncertainty are not going to be available soon.
and more at....
http://www.energyendgame.com/DirtySecret.htm