Attempts to explain the general
or average way that the atmosphere and oceans circulate
and redistribute heat and moisture. These models do not
account for daily variations of the circulation patterns but
look at seasonal and longer term averages. Many general circulation
models attempt to answer fundamental questions
about the motion of the atmosphere, what drives this motion,
and what are its consequences. They may start with input
such as the latitudinal distribution of heating in different seasons,
and try to determine how the atmosphere moves heat
from the equator toward the poles, and also consider the
return flow of cold air from the poles to the equator. Other
inputs to the models would include the distribution of continents
and their uneven heating effects, the influences of
topography on atmospheric circulation, the rotation of the
Earth, and interactions between the oceans and atmosphere.
See also ATMOSPHERE; EL NIÑO; HADLEY CELLS; LA NIÑA.














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