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  2. 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
     
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