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    Inclusion of Rainwater Budget and Convective Downdrafts in the Arakawa–Schubert Cumulus Parameterization

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 010::page 1359
    Author:
    Cheng, Ming-Dean
    ,
    Arakawa, Akio
    DOI: 10.1175/1520-0469(1997)054<1359:IORBAC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A 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.
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      Inclusion of Rainwater Budget and Convective Downdrafts in the Arakawa–Schubert Cumulus Parameterization

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158386
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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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