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Interocean Exchange

Gordon, Arnold L.

Earth’s climate, responding to the different thermodynamic properties of the land and ocean surfaces, is sensitive to the continental configuration and distribution
of mountain ranges. This is clearly seen in the pattern of mean annual and seasonal range in such climate parameters as temperature and humidity and in the quasistationary patterns of atmospheric circulation, from small-scale sea breezes to planetary waves.


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Ocean circulation and climate: observing and modelling the global ocean
Academic Press

More About This Work

Academic Units
Earth and Environmental Sciences
Published Here
April 10, 2013
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