Science is a continual process of observation, understanding, modelling, testing and
prediction. The prediction of a long-term trend in global warming from increasing
greenhouse gases is robust and has been confirmed by a growing body of evidence.
Nevertheless, understanding (for example, of cloud dynamics, and of climate variations
on centennial and decadal timescales and on regional-to-local spatial scales) remains
incomplete. All of these are areas of active research. Comparisons of model predictions with observations identify what is well-understood and, at the same
time, reveal uncertainties or gaps in our understanding. This helps to set priorities for new research.
Vigilant monitoring of the entire climate system—the atmosphere, oceans, land, and ice—is therefore
critical, as the climate system may be full of surprises.
Together, field and laboratory data and theoretical understanding are used to advance models of Earth’s climate
system and to improve representation of key processes in them, especially those associated with clouds,
aerosols, and transport of heat into the oceans. This is critical for accurately simulating climate change and
associated changes in severe weather, especially at the regional and local scales important for policy decisions.
Simulating how clouds will change with warming and in turn may themselves affect warming, remains
one of the major challenges for global climate models, in part because many cloud processes occur on
scales smaller than the current models can resolve. Greater computer power may enable some of these
processes to be resolved in future-generation models.
Dozens of groups and research institutions work on climate models, and scientists are now able to analyse
results from essentially all of the world’s major Earth-System Models and compare them with each other and
with observations. Such opportunities are of tremendous benefit in bringing out the strengths and weaknesses
of various models and diagnosing the causes of differences among models, so that research can focus
on the relevant processes. The differences among models allow estimates to be made of the uncertainties in
projections of future climate change, and in understanding which aspects of these projections are robust.
Studying how climate responded to major changes in the past is another way of checking that we understand
how different processes work and that models are capable of performing under a wide range of conditions. |