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Heat Budget of Earth

Earth and its atmosphere are continuously receiving solar energy. Most of the solar energy reaches the surface of the earth in the form of short waves. Earth absorbs it and converts it into heat. Due to its special temperature, the earth sends the heat absorbed by terrestrial radiation back to the space through long waves.

Earth absorbs black body that means each and everybody whereas atmosphere is very selective, and it absorbs 85% of long waves and it is transparent for short waves, that transparency is known as atmospheric window.

In this way the earth does not store solar energy but sends the same amount of energy back to the space through terrestrial radiation. This exchange of energy is made possible by highly complex processes of radiation. This is the reason why the annual average temperature of the earth's surface remains constant. There is no significant change in it.

Let the temperature received at the upper surface of the atmosphere be 100 units. Out of this, only 51 units of heat reaches the earth. 49 units heat gets reflected in the atmosphere and space. 35 units of heat is converted into space even before reaching the surface of the earth. Out of this, 6 units are scattered in space (by dust-particle), 27 units are reflected by the clouds and 2 units are reflected by snow covered areas (Glacier) on the earth.

This reflected amount of solar radiation is called the Albedo (it is the ratio of incoming solar radiation to the outgoing solar radiation. In case of snow Albedo is 80% whereas in case of land it is 30-35%) of the Earth. Out of the remaining 65 units, 14 units of heat is absorbed by the atmosphere (water vapor). Thus, out of 100 units on the earth, only 51 units of heat reach the surface.
51 units absorbed by the earth are returned back to the atmosphere in the form of terrestrial radiation. Of these, 17 units are directly returned to space and 34 units are absorbed by the atmosphere. Out of these 34 units, 6 units are absorbed by the atmosphere itself, 9 units by convection process and 19 units as latent heat.

48 units absorbed by the atmosphere (14 units from solar heat and 34 units from terrestrial radiation) are returned to space. Thus, the heat received by the earth and its atmosphere is equal to the heat released by them. The balance of heat received by the earth and atmosphere and the loss of heat by them is called heat budget or heat balance.

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