Climate Models: How Good Are They?

The author of today's post, Lisa Moore, is a scientist in the Climate and Air Program.

Stephen Colbert once quipped, "It's not that I don't believe in climate change, it's that I don't believe in climate. Have you ever heard anyone say, "How's the climate?" No! They say, "How's the weather?""

People often confuse climate and weather. They wonder how scientists can reliably predict climate 50 years from now when they can't predict the weather a few weeks from now. The answer is that climate and weather are different, and it's easier to predict climate than weather.

Weather is a short-term, local phenomenon. Climate is the average weather pattern of a region over many years. I may not be able to predict the weather in New York City on December 15, but I can predict with confidence that it will be colder than it is today, in mid-July.

A climate model could make the same prediction without a single past temperature reading. Basic orbital mechanics tell us that the northern hemisphere is colder in winter than summer.

As I explained in my previous post, a climate model is a mathematical description of the physics and chemistry of the climate system – for example, how heat is transferred from one place to another. The inputs to the model are things like solar radiation, volcanic eruptions, and human-produced greenhouse gas emissions. Based on these inputs and the laws of physics, the model predicts temperature, precipitation, and other aspects of climate.

Which brings me to how we know the models are credible.

What if the model inputs were actual observations from a time period in the past where we have full climate measurements? If the model is any good, it should accurately "hindcast" what we know the climate conditions were. In fact, hindcasting is the technique scientists use to evaluate models. If a model can accurately hindcast, we can have some confidence in its forecasts of the future.

In the graph below, the yellow lines show 58 temperature hindcasts from 14 different climate models. The thick red line is the average of all the hindcasts; the black line shows actual global temperature over the past century. Note how close the hindcast average is to actual temperatures. The models do a very good job of predicting 20th century climate.

Source: IPCC AR4 WG1 Figures [PPT file]

Why do we need 14 different models? Models vary in their complexity – how many factors they take into account. A simple model can take just a minute to run, but a complex model requires serious computing power and time. Even complex models differ in the factors they consider.

And how is it that the same model can produce different hindcasts? This has to do with the nature of the grid I described in my previous post. The atmospheric cells used to predict global climate are larger than some of the inputs to the model – for example, clouds. The way scientists take these influences into account is by "parameterizing" these "subgridscale" phenomena – that is, they make an estimate. The different hindcasts come from different parameter assumptions.

Averaging the predictions of different models and different parameters usually gives a better prediction of real-world observations than any one model. The averaging minimizes any bias there may be in a particular approach.

The issue of what to input when forecasting – for example, the level of carbon emissions to expect – can be tricky. Scientists thus look at different scenarios. For example, in the graph below, A2 is the most fossil-fuel intensive scenario and B1 the least. The scenarios [PDF] are based on "storylines" representing different demographic, social, economic, technological, and environmental developments (none of which includes initiatives to decrease greenhouse gas emissions).

Source: Figure SPM-7 in the summary of the latest IPCC report [2.9 MB PDF]

The Year 2000 line shows what happens if greenhouse gas concentrations stay at current levels. Temperatures will continue to rise slightly because it takes some time for carbon emissions to translate into global warming. Scientists call this the "warming in the pipeline".

Note that despite differences and imperfections, the models are unanimous in predicting future warming. To avoid dangerous climate change, temperatures cannot rise more than 2.3°F above what they are today. (For why, see Bill's post on How Warm is Too Warm?.) Even the best business-as-usual scenario ("B1" in blue) crosses that tipping point.

The implication is clear: we must cut our greenhouse gas emissions as soon as
possible. And now you know why scientists have confidence in these models!

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One Comment

  1. Posted July 19, 2007 at 3:20 pm | Permalink

    Global Warming? “No worries,” say two forecasting researchers.

    Kesten Green and J. Scott Armstrong recently examined the validity of the climate forecasts. To date, they have found no scientific forecasts to support global warming. Their paper "Global Warming: Forecasts by Scientists versus Scientific Forecasts" is forthcoming in Energy and Environment. The paper can be found at a new site designed to encourage a scientific approach to forecasting for public policy issues, publicpolicyforecasting.com. Reactions to the paper can be found at theclimatebet.com.

    -Rachel Zibelman on behalf of J. Scott Armstrong

2 Trackbacks

  • [...] A few weeks ago, researchers led by Dr. Stephen Sitch published a paper in Nature titled "Indirect radiative forcing of climate change through ozone effects on the land-carbon sink [PDF]" (paid subscription required) that attempts to quantify the problem on a global scale. Using data from the small-scale experiments, they modified a global-scale carbon cycle model to include the effects of CO2 and ozone on plant CO2 uptake. (See my previous post for more on how climate models work.) Then they ran the model using a business-as-usual scenario of CO2 emissions, with and without projected increases in ozone concentration. [...]

  • [...] A paper in today's issue of Science ("Improved Surface Temperature Prediction for the Coming Decade from a Global Climate Model") describes a new and improved climate model that predicts both greenhouse warming and internal climate variability. The model's hindcasts are substantially better than earlier model results. (For more on hindcasts, see the post "Climate Models: How Good Are They?"). [...]

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