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    An Application of Two Tropical Parameterization Schemes of Convective Latent Heat Release in Middle Latitudes

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 009::page 1141
    Author:
    Edmon, Harold J.
    ,
    Vincent, Dayton G.
    DOI: 10.1175/1520-0493(1976)104<1141:AAOTTP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Models developed by Krishnamurti et al. (1973) and Kuo (1974) for parameterizing the convective latent heat release in synoptic?scale tropical systems are slightly modified and applied to a case study in which Tropical Storm Candy (1968) interacts with a developing extratropical baroclinic frontal system over the United States. Stable latent heat release is also computed, although much of the reported weather activity is unstable. The convective and stable components of latent heat are converted to precipitation rates and compared to the observed precipitation rate. The results show that Krishnamurti's scheme does not produce reliable patterns. Reasons for this failure are discussed. Kuo's scheme, on the other hand, shows better agreement with observed precipitation rates, although discrepancies still exist.
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      An Application of Two Tropical Parameterization Schemes of Convective Latent Heat Release in Middle Latitudes

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199493
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    • Monthly Weather Review

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    contributor authorEdmon, Harold J.
    contributor authorVincent, Dayton G.
    date accessioned2017-06-09T16:01:20Z
    date available2017-06-09T16:01:20Z
    date copyright1976/09/01
    date issued1976
    identifier issn0027-0644
    identifier otherams-58986.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199493
    description abstractModels developed by Krishnamurti et al. (1973) and Kuo (1974) for parameterizing the convective latent heat release in synoptic?scale tropical systems are slightly modified and applied to a case study in which Tropical Storm Candy (1968) interacts with a developing extratropical baroclinic frontal system over the United States. Stable latent heat release is also computed, although much of the reported weather activity is unstable. The convective and stable components of latent heat are converted to precipitation rates and compared to the observed precipitation rate. The results show that Krishnamurti's scheme does not produce reliable patterns. Reasons for this failure are discussed. Kuo's scheme, on the other hand, shows better agreement with observed precipitation rates, although discrepancies still exist.
    publisherAmerican Meteorological Society
    titleAn Application of Two Tropical Parameterization Schemes of Convective Latent Heat Release in Middle Latitudes
    typeJournal Paper
    journal volume104
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1976)104<1141:AAOTTP>2.0.CO;2
    journal fristpage1141
    journal lastpage1153
    treeMonthly Weather Review:;1976:;volume( 104 ):;issue: 009
    contenttypeFulltext
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