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atmospheric temperature
Atmospheric temperature is a measure of temperature at different levels of the Earth's atmosphere. It is governed by many factors, including incoming solar radiation, humidity and altitude. When discussing surface temperature, the annual atmospheric temperature range at any geographical location depends largely upon the type of biome, as measured by the Köppen climate classification.
==Temperature versus height==
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(詳細はEarth's surface. The coldest temperatures lie near the mesopause, an area approximately to above the surface. In contrast, some of the warmest temperatures can be found in the thermosphere, which receives strong ionizing radiation at the level of the Van Allen radiation belt.
Temperature varies as one moves vertically upwards from the Earth's Surface.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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