Mechanisms of cloud-radiation interaction in the tropics and midlatitudes

The results of a study indicate that the dominant process for enhancing the surface precipitation in both the PRESTORM and EMEX squall cases is the large-scale radiative cooling.

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Bibliographische Detailangaben
Veröffentlicht in:	Journal of the atmospheric sciences 1996-09, Vol.53 (18), p.2624-2651
Hauptverfasser:	TAO, W.-K, LANG, S, SIMPSON, J, SUI, C.-H, FERRIER, B, CHOU, M.-D
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmosphere Clouds Earth, ocean, space Exact sciences and technology External geophysics Meteorology Radiation Rain Solar energy Storms, hurricanes, tornadoes, thunderstorms Tropical environments
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Beschreibung
Zusammenfassung:	The results of a study indicate that the dominant process for enhancing the surface precipitation in both the PRESTORM and EMEX squall cases is the large-scale radiative cooling.
ISSN:	0022-4928 1520-0469
DOI:	10.1175/1520-0469(1996)053<2624:mocrii>2.0.co;2