Abstract
For land areas, precipitation is one of the most important processes for the biosphere, including mankind. For the oceans, precipitation is a source for freshwater and thus an important forcing term for the thermohaline circulation. In the atmosphere, precipitation liberates latent energy, which is a main forcing term for atmospheric motions, especially in the tropics. The global average precipitation is equivalent to a water column of about 1m height. This amounts to a continuous energy supply to the atmosphere of about 80 Wm-2, which is roughly 30% of the incoming solar energy. Mainly caused by its strong coupling to the vertical velocity field, precipitation is extremely variable in space and time.
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© 1996 Springer-Verlag Berlin Heidelberg
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Simmer, C. (1996). Retrieval of Precipitation from Satellites. In: Raschke, E. (eds) Radiation and Water in the Climate System. Nato ASI Series, vol 45. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-03289-3_11
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DOI: https://doi.org/10.1007/978-3-662-03289-3_11
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