Changes in the planetary heat balance with chemical changes in air

Details Changes in the planetary heat balance with chemical changes in air Changes in the planetary heat balance with chemical changes in air

Nov 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980p%26ss...28.1011c&link_type=abstract

Planetary and Space Science, vol. 28, Nov. 1980, p. 1011-1018. NASA-NSF-supported research;

Computer Science

3

Atmospheric Chemistry, Atmospheric Heat Budget, Atmospheric Models, Radiative Heat Transfer, Atmospheric Composition, Atmospheric Moisture, Carbon Dioxide Concentration

Scientific paper

The concept of an 'equivalent radiative atmosphere', a simplified model of the atmospheric radiative aspects, is used to explore changes in the greenhouse effect, caused by changes in the atmospheric composition, and changes in the incident solar flux. By extending this model to the zonal energy-balance type, it is shown that global heating has the more profound effect at higher latitudes. It is also shown that the positive feedback in H2O opacity is comparable to the initial change in opacity due, for example, to a change in CO2 content.

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