The skin temperature of an atmosphere is the temperature of a hypothetical thin layer high in the atmosphere that is transparent to incident solar radiation and partially absorbing of infrared radiation from the planet. It provides an approximation for the temperature of the tropopause on terrestrial planets with greenhouse gases present in their atmospheres. The skin temperature of an atmosphere should not be confused with the surface skin temperature, which is more readily measured by satellites, and depends on the thermal emission at the surface of a planet.
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