A
brief history of models
CCSM
belongs to an elite category of computer-based simulations known as general-circulation
models. Such models use mathematical formulas to recreate the chemical
and physical processes that drive Earth’s climate. Extraordinarily
sophisticated, they incorporate phenomena ranging from the effect that
volcanic eruptions have on temperature patterns to the impact of shifting
sea ice on sunlight in the atmosphere. What emerges from trillions of
computer calculations is a picture of the world’s climate in all
its complexity.
Models such as CCSM are vital to climate science because researchers cannot
recreate the atmosphere in a test tube and run experiments on it. Instead,
since the 1950s, scientists have used increasingly sophisticated computer
programs to answer our most fundamental climate questions, such as the
impact of El Niño on North American rainfall and the effect industrial
pollution has on temperature and precipitation. As they become more powerful,
these models eventually will help us predict the likelihood of climate
patterns for specific regions or individual states, providing information
that government and business leaders can use to protect investments—and
even save lives.
Climate
modeling has its roots in the 1950s, when meteorologists tracking daily
weather turned to the first vacuum-tube computers to try to forecast variables
such as temperature, wind, and humidity. As technology advanced, model
simulations were carried out for longer time scales, thus giving birth
to climate models. Researchers created models using classical physics
equations, such as the conservation of momentum and heat, to shed light
on the average state of the entire atmosphere over long time periods.
The resulting general circulation models, by the 1970s, emerged as a central
tool of climate science.
Meanwhile, oceanographers created computer models of their own to simulate
general circulation in the oceans. Since ocean currents and temperatures
are a major component of the overall climate system, climatologists began
"coupling" ocean and atmosphere models in the 1980s.
To
mimic climate even more accurately, scientists in the last 15 years or
so have turned to increasingly powerful supercomputers to incorporate
additional pieces of Earth’s climate system, including sea ice and
land. Today’s models represent a staggeringly complex effort to
simulate natural events that may occur hourly (large frontal systems),
monthly (jet-stream meanders), or even on timescales of decades or centuries
(ocean circulation and glacial changes).
Climatologists around the world have created about a dozen fully coupled
atmosphere-ocean models. Some of the better known models, in addition
to CCSM, have been developed by Britain’s Hadley Centre for Climate
Prediction and Research and Germany’s Max Planck Institute for Meteorology.
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