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    Inversion Methods of Three Cumulus Parameterizations for Diabatic Initialization of a Tropical Cyclone Model

    Source: Monthly Weather Review:;1996:;volume( 124 ):;issue: 010::page 2304
    Author:
    Kasahara, Akira
    ,
    Tsutsui, Jun-Ichi
    ,
    Hirakuchi, Hiromaru
    DOI: 10.1175/1520-0493(1996)124<2304:IMOTCP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: To generate convective precipitation consistent with observations at the beginning of a forecast with an atmospheric prediction model, the irrotational circulation and moisture fields must be initialized properly for dynamical balance with the input rotational and mass fields. This article describes a diabatic initialization procedure for a tropical cyclone forecast model, including the adjustment of the input moisture field with the use of ?observed? precipitation data from satellites. The condensation heating rate estimated from ?observed? precipitation data and the radiative heating rate calculated from the input data are used as the diabatic heat source to calculate the balanced irrotational wind field using a diabatic nonlinear normal mode initialization algorithm. The adjustment of the moisture field is performed by the inversion of cumulus parameterization, knowing the input precipitation rate. The inversion methods of three cumulus parameterization schemes are presented. The three cumulus schemes considered here are the Kuo scheme modified by R. Anthes, the relaxed Arakawa?Schubert scheme developed by S. Moorthi and M. Suarez, and a mass-flux scheme formulated by J. Hack. The diabatic and moisture initialization procedures are tested using a regional model for prediction of Typhoons Ed and Flo in the western Pacific during September 1990. The regional prediction model is an augmented version of the Pennsylvania State University?NCAR mesoscale model. The combined diabatic and cumulus initialization can ameliorate the problem of precipitation spinup. However, the adjusted moisture state after cumulus initialization differs considerably, depending on which cumulus parameterization is used. The inversion of cumulus parameterization requires the information of sensitivity of precipitation rate δP to a small variation of moisture δq. The sensitivity δP/δq is a measure for the behavior of different cumulus parameterizations.
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      Inversion Methods of Three Cumulus Parameterizations for Diabatic Initialization of a Tropical Cyclone Model

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4203729
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    • Monthly Weather Review

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    contributor authorKasahara, Akira
    contributor authorTsutsui, Jun-Ichi
    contributor authorHirakuchi, Hiromaru
    date accessioned2017-06-09T16:11:01Z
    date available2017-06-09T16:11:01Z
    date copyright1996/10/01
    date issued1996
    identifier issn0027-0644
    identifier otherams-62798.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203729
    description abstractTo generate convective precipitation consistent with observations at the beginning of a forecast with an atmospheric prediction model, the irrotational circulation and moisture fields must be initialized properly for dynamical balance with the input rotational and mass fields. This article describes a diabatic initialization procedure for a tropical cyclone forecast model, including the adjustment of the input moisture field with the use of ?observed? precipitation data from satellites. The condensation heating rate estimated from ?observed? precipitation data and the radiative heating rate calculated from the input data are used as the diabatic heat source to calculate the balanced irrotational wind field using a diabatic nonlinear normal mode initialization algorithm. The adjustment of the moisture field is performed by the inversion of cumulus parameterization, knowing the input precipitation rate. The inversion methods of three cumulus parameterization schemes are presented. The three cumulus schemes considered here are the Kuo scheme modified by R. Anthes, the relaxed Arakawa?Schubert scheme developed by S. Moorthi and M. Suarez, and a mass-flux scheme formulated by J. Hack. The diabatic and moisture initialization procedures are tested using a regional model for prediction of Typhoons Ed and Flo in the western Pacific during September 1990. The regional prediction model is an augmented version of the Pennsylvania State University?NCAR mesoscale model. The combined diabatic and cumulus initialization can ameliorate the problem of precipitation spinup. However, the adjusted moisture state after cumulus initialization differs considerably, depending on which cumulus parameterization is used. The inversion of cumulus parameterization requires the information of sensitivity of precipitation rate δP to a small variation of moisture δq. The sensitivity δP/δq is a measure for the behavior of different cumulus parameterizations.
    publisherAmerican Meteorological Society
    titleInversion Methods of Three Cumulus Parameterizations for Diabatic Initialization of a Tropical Cyclone Model
    typeJournal Paper
    journal volume124
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1996)124<2304:IMOTCP>2.0.CO;2
    journal fristpage2304
    journal lastpage2321
    treeMonthly Weather Review:;1996:;volume( 124 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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