Climate Models Don't Predict Climate
In recent years, climate models have had as their most prominent use the projection of climate for the next century or two under certain scenarios. These scenarios have two main parts: behavior of humans and behavior of polar ice sheets. The human behavior has three major parts; greenhouse gas concentrations, land use changes, and aerosol (dust) emissions. These in turn can be broken down further, but that's beside my point for now. And then there's the ice sheets, whose behavior is greatly hoped to be "nothing much", but is increasingly suspected to be something other than that.
The greenhouse gas concentrations themselves aren't quantities that even social and economic projections can give us. What economists try to offer is some sort of projection of emissions scenarios, that is, the amount of gas spewed into the air per year. There is some chemistry (including biochemistry) between those emissions and the actual concentrations (total amount in the air at any instant) over time. That chemistry is very poorly understood. We can identify most of the processes at work, we think, but we cannot quantify them very well even under current conditions.
So when we run the climate models into the future, there is a lot of guesswork about what conditions the climate system will be under. (For somewhat mathematical and somewhat historical reasons we tend to call these conditions "boundary conditions"; they're related to but not exactly the same as the boundary conditions you'll encounter if you study partial differential equations.) We can be pretty sure it isn't a realistic bet of the boundary conditions. Even so, when different models are run under identical scenarios, you'd hope they would get the same answer. (This is a useful sanity check if nothing else.) Well, what comes out is in some ways similar across models, but there are many differences. Models tend to agree that Arizona will get drier and Scotland wetter. They are literally all over the map when it comes to soil moisture in Texas, though.
I've recently come across a small group of people who seem to take great glee in finding technical problems with these models. I personally agree with some of their complaints though without much pleasure. I have to use the darned things myself.
Their main point, though, is that important decisions are based on these models. That point, though, isn't really true.
I think that the only important decision that climate models yet have any direct bearing on is whether greenhouse gases need to be curtailed, and even then the impact is more in the way of confirmation rather than motivation. We know the radiative properties of the atmosphere are changing as a result of human activity. We know that such changes are a primary factor in how the atmosphere behaves. We have, therefore three choices (you can pick all in combination, or just one, but you can't pick none of them) 1) accelerating climate change 2) large cutback in emissions and 3) artificial mechanisms to remove greenhouse gases from the air. The climate models don't really have much to say about how much, when, or how, which are really the big questions.
So what are the models for? Should we improve the effort or should we give it up?
It turns out the press and the public are very confused about the role of the models, and the modeling centers are complicit in this confusion. The projections that give us the scary maps we often see in the press are pretty much of the right magnitude, but the details are still crude and the costs are pretty high.
See, the models aren't really for the policy sector. They are for the scientists. Their most prominent use is not their most important use. I'll explain more next time.







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2 Comments
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March 31, 2008 10:16 PM
Alexi Tekhasski
Michael, you stated:
"We know the radiative properties of the atmosphere are changing as a result of human activity. We know that such changes are a primary factor in how the atmosphere behaves."
How did you conclude that these factors are primary?
Could you consider the following quasi-realistic initial conditions. Let say you have a globe with completely dry atmosphere, and no other greenhouse gases are present, ever. Let say that the oceans and lands have been initially isolated from the atmosphere, and the Earth has reached a steady state balance with incoming solar radiation, which is supposed to lead to 255K average surface temperature.
Now, you remove the isolation at t=0, so the water surface is free to evaporate in accord with Clausius-Clapeyron boundary condition. Could you tell us how a typical climate model will evolve in time? What will happen to surface temperatures? Obviously, initial evaporation will add some vapor to the air, so some greenhouse effect must develop. What will happen then?
Thanks,
- Alexi
April 1, 2008 12:01 PM
Michael Tobis
Hi, Alexi. Offer of a personal meeting over coffee stands. My treat. I believe we ought to be able to reach a less adversarial and more productive way of discussing these matters. Meanwhile I am not sure what trap you are trying to set for me here, but what the heck, I will walk into it.
You ask "How did you conclude that these factors are primary?"
Multiple streams of evidence, theoretical and observational. It's really a crucial feature of the atmosphere.
Note that I said "a primary" not "the primary". I consciously shied away from "first order" as well, partly in deference to a broad audience but partly in deference to the likes of you who might bring up a drawn out argument about it.
If it helps, I will freely concede that a doubling in solar output, say, will have a larger effect than a doubling in greenhouse gases.
Your experiment is incompletely specified; you need to specify the lower boundary of the atmosphere in the first half and the initial sea surface temperature in the second half. It is possible to argue that the consistent sea surface temperature is such that the ocean would be frozen. Hence not very much would happen at all in a "typical" model that does not extend to time scales where volcanic sources of carbon dioxide would be included, and anyway you have excluded CO2 altogether.
That said, suppose we move the whole system a little closer to the sun so it doesn't freeze, which I think is the question you are trying to ask.
You would still begin with a quiescent atmosphere with a steep temperature gradient; the lack of cloud physics in the initial system would produce something very unlike the terrestrial atmosphere. (As I mentioned in a previous article, the presence of a methane ocean on Titan has created a much more earthlike circulation there than on any other observable "planet" (where by planet I mean a solid body with an atmosphere).)
The spinup from the one state to the other would be vastly complicated and it's very difficult to know what physics to include or not.
Perhaps you'd rather propose an experiment where a slab ocean is replacd by a dynamic ocean, to make your point?
All that said, if you are trying to say that the coupled system would introduce new dynamics, I agree.
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