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Through conduction: the transfer of energy from matter touching another matter.
It's warmed from the surface. Shortwave radiation passes through the atmosphere, or at least about half of it, where it reaches the ground and is absorbed. The ground re-emits it at a longer wavelength, thereby warming the lower atmosphere.
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.
decreases i think
The atmosphere helps keep earth's surface warm, but does not generate heat itself. The earth is warmed primarily by solar radiation (heat from the sun), and to a lesser extent by the slow decay of long lived heavy isotopes within earth's mantle and core.
Through conduction: the transfer of energy from matter touching another matter.
It's warmed from the surface. Shortwave radiation passes through the atmosphere, or at least about half of it, where it reaches the ground and is absorbed. The ground re-emits it at a longer wavelength, thereby warming the lower atmosphere.
A small part of the heating of the atmosphere is directly from the sun. A lot of heating near the surface is done through conduction from land or water that has been warmed by the sun.
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.
The sun
themosphere
The suns energy
Warm front
decreases i think
The sun can only shine on part of the earth's surface at any one time. This is why we have day and night in a rolling approach as the earth rotates.
The atmosphere helps keep earth's surface warm, but does not generate heat itself. The earth is warmed primarily by solar radiation (heat from the sun), and to a lesser extent by the slow decay of long lived heavy isotopes within earth's mantle and core.
The atmosphere helps keep earth's surface warm, but does not generate heat itself. The earth is warmed primarily by solar radiation (heat from the sun), and to a lesser extent by the slow decay of long lived heavy isotopes within earth's mantle and core.