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contributor authorCheng, Ming-Dean
contributor authorArakawa, Akio
date accessioned2017-06-09T14:34:30Z
date available2017-06-09T14:34:30Z
date copyright1997/05/01
date issued1997
identifier issn0022-4928
identifier otherams-21987.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158386
description abstractA combined updraft?downdraft model that includes the mass, rainwater, and vertical momentum budget equations for both updrafts and downdrafts is incorporated into the Arakawa?Schubert (A?S) cumulus parameterization. The model assumes that the rainwater generated in an updraft falls partly inside and partly outside the updraft. Two types of stationary solutions are identified for the coupled rainwater budget and vertical momentum equations: solutions for small tilting angles and solutions for large tilting angles. The balance of terms in the rainwater budget equation is quite different between these solutions, and solutions for small tilting angles are unstable, while solutions for large tilting angles are stable. The cause of the instability is interpreted, considering the effect of rain drag on the vertical transport of rainwater. The motivation for an optimum choice of the tilting angle for use in the revised parameterization is discussed. The results of semiprognostic and single-column prognostic tests of the revised A?S parameterization using the GATE Phase III data show drastic improvement in predicting the humidity field through the inclusion of downdraft effects. An updraft model with a simplified rainwater budget equation, which is used in the authors? current GCM applications of the revised parameterization, is also presented.
publisherAmerican Meteorological Society
titleInclusion of Rainwater Budget and Convective Downdrafts in the Arakawa–Schubert Cumulus Parameterization
typeJournal Paper
journal volume54
journal issue10
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1997)054<1359:IORBAC>2.0.CO;2
journal fristpage1359
journal lastpage1378
treeJournal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 010
contenttypeFulltext


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