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contributor authorEshel, Gidon
contributor authorFarrell, Brian F.
date accessioned2017-06-09T14:36:40Z
date available2017-06-09T14:36:40Z
date copyright2001/01/01
date issued2001
identifier issn0022-4928
identifier otherams-22761.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159247
description abstractThis note focuses on thermodynamic changes caused by Eastern Mediterranean (EM) subsidence anomalies. Subsidence anomalies are shown to modulate EM-wide stability with respect to moist ascent. Additionally, convective available potential energy (CAPE) generation rates, as well as mean CAPE, change coherently during extreme EM rainfall anomalies. It is suggested that the resulting modulation of convective rain generation is the process directly responsible for the observed rainfall anomalies.
publisherAmerican Meteorological Society
titleThermodynamics of Eastern Mediterranean Rainfall Variability
typeJournal Paper
journal volume58
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(2001)058<0087:TOEMRV>2.0.CO;2
journal fristpage87
journal lastpage92
treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 001
contenttypeFulltext


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