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Full colour version of the BP magazine

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The Big Issue<br />

CLIMATE MODELS: FORECASTING THE FUTURE<br />

Climate models increasingly help us understand<br />

<strong>the</strong> reasons behind climate change and what might<br />

happen in <strong>the</strong> future. Scientists<br />

from <strong>the</strong> Met Office discuss <strong>the</strong><br />

benefit <strong>of</strong> having this knowledge.<br />

Climate is something different from<br />

wea<strong>the</strong>r. The difference is <strong>of</strong>ten<br />

described as climate being <strong>the</strong> kind<br />

<strong>of</strong> wea<strong>the</strong>r patterns you might expect, while<br />

wea<strong>the</strong>r is <strong>the</strong> conditions you get on any<br />

given day. However, both need complex<br />

computer models to make predictions.<br />

There is considerable scientific evidence<br />

that <strong>the</strong> world’s climate is changing and<br />

that we are responsible for most <strong>of</strong> <strong>the</strong> recent<br />

acceleration in warming. Climate models help us<br />

understand <strong>the</strong> causes <strong>of</strong> climate change and provide<br />

<strong>the</strong> means to assess a range <strong>of</strong> likely future changes. For<br />

example, we know some change is inevitable; but we<br />

need to know how sensitive <strong>the</strong> climate is to greenhouse<br />

gases so we can adapt to those variations. Climate<br />

projections will also help identify changes which are<br />

avoidable if we act to reduce our greenhouse gas emissions.<br />

Because <strong>the</strong> Earth’s climate is highly complex, huge<br />

supercomputers are needed to make <strong>the</strong>se kinds <strong>of</strong><br />

projections. Our climate models represent <strong>the</strong> physical,<br />

chemical and biological processes <strong>of</strong> <strong>the</strong> atmosphere, ocean, and<br />

biosphere, and how each system reacts with <strong>the</strong> o<strong>the</strong>rs.<br />

Ma<strong>the</strong>matical equations are solved by a computer programme on<br />

a 3D lattice <strong>of</strong> grid points which cover <strong>the</strong> globe. Such a ‘virtual<br />

Earth’ is used for experiments to examine <strong>the</strong> effects <strong>of</strong> different<br />

influences – both human-induced and naturally occurring – to<br />

explain <strong>the</strong> causes <strong>of</strong> past climate changes, and make future<br />

projections under different scenarios <strong>of</strong> greenhouse gas emissions.<br />

Limited projections<br />

As in every field <strong>of</strong> science, <strong>the</strong>re are uncertainties in climate<br />

projections. Much is still not known about how <strong>the</strong> climate system<br />

works: for instance, we have an incomplete understanding <strong>of</strong> icesheet<br />

dynamics and so, <strong>the</strong>refore, we are uncertain about <strong>the</strong> rates<br />

at which glaciers will melt and slide into <strong>the</strong> sea. Projections are<br />

also limited by available computing resources, which restricts <strong>the</strong><br />

number and detail <strong>of</strong> <strong>the</strong> processes that can be represented.<br />

In spite <strong>of</strong> <strong>the</strong> limitations <strong>of</strong> computer power, we are steadily<br />

improving our understanding <strong>of</strong> <strong>the</strong> atmosphere and its<br />

interactions with <strong>the</strong> ocean and biosphere. In <strong>the</strong> 1970s, carbon<br />

dioxide concentrations, <strong>the</strong>ir warming impact and rain were<br />

included in climate models, but not <strong>the</strong> effect <strong>of</strong> clouds. Nor did<br />

those models capture <strong>the</strong> interactions <strong>of</strong> <strong>the</strong> atmosphere with <strong>the</strong><br />

ocean and biosphere. Today’s state-<strong>of</strong>-<strong>the</strong>-art models include a far<br />

more complete and interactive treatment <strong>of</strong> clouds and aerosols,<br />

as well <strong>the</strong> coupling <strong>of</strong> <strong>the</strong> atmosphere to oceans and ecosystems.<br />

Fur<strong>the</strong>r research will see this improvement continue.<br />

More sophisticated models are starting to include more <strong>of</strong> <strong>the</strong><br />

detailed chemistry <strong>of</strong> <strong>the</strong> carbon cycle, enabling <strong>the</strong> modeller to<br />

06 Issue 1 2009 <strong>BP</strong> MAGAZINE<br />

consider whe<strong>the</strong>r plants, soils and oceans will absorb less carbon<br />

as warming continues. Future computer models will include<br />

refined atmospheric processes and a wider range <strong>of</strong> feedback<br />

mechanisms that may contribute to climate change.<br />

These models enable projections <strong>of</strong> future climate and <strong>the</strong><br />

investigation <strong>of</strong> reasons for changes in <strong>the</strong> geological past<br />

(paleoclimate). As information from geological observations fills<br />

in <strong>the</strong> picture, models <strong>of</strong> <strong>the</strong> atmosphere are constrained and<br />

improved. If <strong>the</strong> aim is to assess vulnerabilities to climate change<br />

and prepare for changes in general, climate models can only go so<br />

far. The spatial or temporal resolution required for certain<br />

assessments may be finer than <strong>the</strong> models can currently resolve,<br />

and interpreting <strong>the</strong> results in <strong>the</strong> context <strong>of</strong> <strong>the</strong> application still<br />

presents a significant scientific challenge.<br />

Added benefits<br />

However, climate modelling is not exclusively reserved for policy<br />

guidance. The Met Office Hadley Centre climate model<br />

(HadGEM3) is unique in using <strong>the</strong> same basic model for wea<strong>the</strong>r<br />

forecasting and projections <strong>of</strong> climate change. The Met Office has<br />

extended its forecasting to seasonal, decadal and centennial<br />

timescales. In seasonal forecasting, recent developments in<br />

tropical storm and wave-height modelling have brought added<br />

benefits to <strong>the</strong> oil and gas industry; and on longer scales, climate<br />

models are being used to explore new threats and opportunities<br />

to <strong>the</strong> industry, such as changes in permafrost regimes.<br />

For more information on <strong>the</strong> development <strong>of</strong> climate<br />

modelling and how Princeton University is using it to better<br />

understand <strong>the</strong> nature <strong>of</strong> climate change, see pages 48-51. ■<br />

Illustration: David Lyttleton

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