Absorption equilibrium of solar radiation between the two hemispheres of Earth

Details Absorption equilibrium of solar radiation between the two hemispheres of Earth Absorption equilibrium of solar radiation between the two hemispheres of Earth

Aug 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980aesr.book.....n&link_type=abstract

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Astronomy and Astrophysics

Astronomy

Climatology, Cloud Cover, Earth Albedo, Radiation Absorption, Solar Radiation, Continents, Latent Heat, Latitude, Oceans

Scientific paper

The absorption of solar radiation by the Earth is a function of astronomical parameters (height, distance from the Sun) and of terrestrial parameters (albedo, bio-albedo, latent heat). The distribution of ocean and land may induce a disequilibrium of the solar radiation absorption between both hemispheres. The energy intake calculated by latitude zone, taking into account the global cloud cover, shows the balance between both hemispheres due to climate feedback processes.

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