Absorption Equilibrium of Solar Radiation Between the Two Hemispheres of Earth Equilibrio DA Absorcao DA Radiacao Solar Entre OS Dois Hemisferios DA Terra

摘要

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.