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    Heat and Moisture Budget Analyses Using BOMEX Data

    Source: Monthly Weather Review:;1974:;volume( 102 ):;issue: 001::page 17
    Author:
    Nitta, Tsuyoshi
    ,
    Esbensen, Steven
    DOI: 10.1175/1520-0493(1974)102<0017:HAMBAU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Large-scale heat and moisture budgets over the tropical Atlantic Ocean are examined during Phase 3 (22?30 June 1969) of the Barbados Oceanographic and Meteorological Experiment (BOMEX). From the satellite cloud photographs of ATS-3, the analyzed period is subdivided into an undisturbed part and a disturbed part. During the undisturbed period, downward motion predominates from the surface to about 500 mb and a large apparent heat sink and apparent moisture source are found near the top of the trade inversion layer. The upward heat flux due to cumulus clouds is confined below the 700-mb level. On the other hand during the relatively disturbed period, upward motion takes place at low levels and the heat flux due to cumulus convection extends to at least 500 mb. Values of the total heat flux estimated by large-scale budgets agree well with those obtained independently by bulk aerodynamic computations.
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      Heat and Moisture Budget Analyses Using BOMEX Data

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199083
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    • Monthly Weather Review

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    contributor authorNitta, Tsuyoshi
    contributor authorEsbensen, Steven
    date accessioned2017-06-09T16:00:28Z
    date available2017-06-09T16:00:28Z
    date copyright1974/01/01
    date issued1974
    identifier issn0027-0644
    identifier otherams-58616.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199083
    description abstractLarge-scale heat and moisture budgets over the tropical Atlantic Ocean are examined during Phase 3 (22?30 June 1969) of the Barbados Oceanographic and Meteorological Experiment (BOMEX). From the satellite cloud photographs of ATS-3, the analyzed period is subdivided into an undisturbed part and a disturbed part. During the undisturbed period, downward motion predominates from the surface to about 500 mb and a large apparent heat sink and apparent moisture source are found near the top of the trade inversion layer. The upward heat flux due to cumulus clouds is confined below the 700-mb level. On the other hand during the relatively disturbed period, upward motion takes place at low levels and the heat flux due to cumulus convection extends to at least 500 mb. Values of the total heat flux estimated by large-scale budgets agree well with those obtained independently by bulk aerodynamic computations.
    publisherAmerican Meteorological Society
    titleHeat and Moisture Budget Analyses Using BOMEX Data
    typeJournal Paper
    journal volume102
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1974)102<0017:HAMBAU>2.0.CO;2
    journal fristpage17
    journal lastpage28
    treeMonthly Weather Review:;1974:;volume( 102 ):;issue: 001
    contenttypeFulltext
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