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    Thermal Budget of a Monsoon Depression in the Bay of Bengal during FGGE-MONEX 1979

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 001::page 242
    Author:
    Saha, Kshudiram
    ,
    Saha, Suranjana
    DOI: 10.1175/1520-0493(1988)116<0242:TBOAMD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The paper presents die results of a study of the thermal budget of a monsoon depression that developed over the Bay of Bengal during the period 3?8 July 1979. The complete thermodynamic energy equation is considered, to examine the possible role of the various terms and to evaluate the total diabatic heating. In the west-southwest quadrant of the monsoon depression where there is considerable rainfall, latent heat released by precipitation appears to account for about 80% of the total diabatic heating. This heating appears to be offset by cooling due to strong upward motion; however, the total diabatic beating over an area immediately to the north-northeast of the depression center appears to be negative, suggesting downward air motion and adiabatic warming. It is suggested that this warm sector to the north-northeast of the depression center, which is maintained by subsidence warming may serve as an effective tropospheric energy source for the monsoon depression.
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      Thermal Budget of a Monsoon Depression in the Bay of Bengal during FGGE-MONEX 1979

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4201933
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    contributor authorSaha, Kshudiram
    contributor authorSaha, Suranjana
    date accessioned2017-06-09T16:06:42Z
    date available2017-06-09T16:06:42Z
    date copyright1988/01/01
    date issued1988
    identifier issn0027-0644
    identifier otherams-61181.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201933
    description abstractThe paper presents die results of a study of the thermal budget of a monsoon depression that developed over the Bay of Bengal during the period 3?8 July 1979. The complete thermodynamic energy equation is considered, to examine the possible role of the various terms and to evaluate the total diabatic heating. In the west-southwest quadrant of the monsoon depression where there is considerable rainfall, latent heat released by precipitation appears to account for about 80% of the total diabatic heating. This heating appears to be offset by cooling due to strong upward motion; however, the total diabatic beating over an area immediately to the north-northeast of the depression center appears to be negative, suggesting downward air motion and adiabatic warming. It is suggested that this warm sector to the north-northeast of the depression center, which is maintained by subsidence warming may serve as an effective tropospheric energy source for the monsoon depression.
    publisherAmerican Meteorological Society
    titleThermal Budget of a Monsoon Depression in the Bay of Bengal during FGGE-MONEX 1979
    typeJournal Paper
    journal volume116
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1988)116<0242:TBOAMD>2.0.CO;2
    journal fristpage242
    journal lastpage255
    treeMonthly Weather Review:;1988:;volume( 116 ):;issue: 001
    contenttypeFulltext
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