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    A Diagnostic Evaluation of Rainfall Predictability for Tropical Storm Agnes, June 1972

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 003::page 363
    Author:
    Carr, Frederick H.
    ,
    Bosart, Lance F.
    DOI: 10.1175/1520-0493(1978)106<0363:ADEORP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The problem of rainfall prediction for a tropical storm over the United States is examined from a diagnostic point of view. A moisture budget is constructed and the differences between the computed and observed precipitation are discussed. Although the areal averages were comparable, the point-by-point agreement was only fair. Stable and convective precipitation are then computed using methods common to many numerical models. The discrepancies between forecast and observed precipitation is assumed to be due to the incomplete formulation of the amount of moisture available for convection. This leads to an expression for the subgrid-scale moisture supply that provides the missing precipitation. Methods are then suggested in which the deficiencies of a parameterization scheme could be corrected during its use in a prognostic model.
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      A Diagnostic Evaluation of Rainfall Predictability for Tropical Storm Agnes, June 1972

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199805
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    • Monthly Weather Review

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    contributor authorCarr, Frederick H.
    contributor authorBosart, Lance F.
    date accessioned2017-06-09T16:01:57Z
    date available2017-06-09T16:01:57Z
    date copyright1978/03/01
    date issued1978
    identifier issn0027-0644
    identifier otherams-59266.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199805
    description abstractThe problem of rainfall prediction for a tropical storm over the United States is examined from a diagnostic point of view. A moisture budget is constructed and the differences between the computed and observed precipitation are discussed. Although the areal averages were comparable, the point-by-point agreement was only fair. Stable and convective precipitation are then computed using methods common to many numerical models. The discrepancies between forecast and observed precipitation is assumed to be due to the incomplete formulation of the amount of moisture available for convection. This leads to an expression for the subgrid-scale moisture supply that provides the missing precipitation. Methods are then suggested in which the deficiencies of a parameterization scheme could be corrected during its use in a prognostic model.
    publisherAmerican Meteorological Society
    titleA Diagnostic Evaluation of Rainfall Predictability for Tropical Storm Agnes, June 1972
    typeJournal Paper
    journal volume106
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1978)106<0363:ADEORP>2.0.CO;2
    journal fristpage363
    journal lastpage374
    treeMonthly Weather Review:;1978:;volume( 106 ):;issue: 003
    contenttypeFulltext
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