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- Temperature patterns in the atmosphere are primarily determined by the amount of sunlight that is absorbed by the surface of the Earth, and the amount of heat that is re-radiated in the atmosphere by the greenhouse gases. Atmospheric and ocean circulation redistribute heat across the surface of the Earth and shape regional temperature patterns1. According to the International Civil Aviation Organization, the standard atmosphere has a temperature of 15 o C at the surface, a lapse rate of 6.5 o C km –1 from 0 km to 11 km, a zero lapse rate from 11 km to 20 km, and a lapse rate of –1 o C km –1 from 20 km to 32 km in the stratosphere2.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Air and water temperatures are primarily determined by the amount of sunlight that is absorbed by the surface of the Earth, and the amount of heat that is re-radiated in the atmosphere by the greenhouse gases. Atmospheric and ocean circulation redistribute heat across the surface of the Earth and shape regional temperature patterns.ugc.berkeley.edu/background-content/temperature/According to the International Civil Aviation Organization (Doc 7488-CD, 1993), the standard atmosphere has a temperature of 15 o C at the surface, a lapse rate of 6.5 o C km –1 from 0 km to 11 km, a zero lapse rate from 11 km to 20 km, and a lapse rate of –1 o C km –1 from 20 km to 32 km in the stratosphere (i.e., temperature increases with height).www.e-education.psu.edu/meteo300/node/594 - People also ask
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