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    On the Onset Vortex of the Summer Monsoon

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 002::page 344
    Author:
    Krishnamurti, T. N.
    ,
    Ardanuy, Philip
    ,
    Ramanathan, Y.
    ,
    Pasch, Richard
    DOI: 10.1175/1520-0493(1981)109<0344:OTOVOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper we examine the evolution of the low-level flow over the Arabian Sea during the onset of the summer monsoon. A detailed examination of the onset vortex that forms over the Arabian Sea just prior to the commencement of heavy rains over central India is carried out. The unique aspect of this study is the use of data sets from the Global Atmospheric Research Program (GARP) Monsoon Experiment (MONEX) from a variety of observing platforms. These include winds from geostationary satellites, constant level balloons, dropwindsonde aircraft and an enhanced World Weather Watch network. The data sets were analyzed for a 46-day period from 16 May through 30 June 1979. A number of calculations were performed with this analysis. Of major interest is a finding that the kinetic energy of the zonal flow over the central Arabian Sea increases by an order of magnitude one week prior to the commencement of monsoon rain over central India. This study provides a MONEX time-averaged analysis for the low-level flow which is an update on the well-known Findlater analysis. A number of calculations show that the horizontal shear of the monsoon current provides substantial energy during the evolution of the onset vortex. The flow satisfies the necessary condition for the existence of instability. Corresponding stability diagrams exhibit substantial growth rates around the period of the formation of the onset vortex. The scale of maximum growth rate is closely in correspondence with the scale of the onset vortex. Finally, the conversion from zonal to eddy kinetic energy is demonstrated via a simple prediction experiment with the conservation of absolute vorticity as a constraint. A reasonable simulation of the onset vortex is shown in this experiment.
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      On the Onset Vortex of the Summer Monsoon

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    contributor authorKrishnamurti, T. N.
    contributor authorArdanuy, Philip
    contributor authorRamanathan, Y.
    contributor authorPasch, Richard
    date accessioned2017-06-09T16:03:16Z
    date available2017-06-09T16:03:16Z
    date copyright1981/02/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59818.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200418
    description abstractIn this paper we examine the evolution of the low-level flow over the Arabian Sea during the onset of the summer monsoon. A detailed examination of the onset vortex that forms over the Arabian Sea just prior to the commencement of heavy rains over central India is carried out. The unique aspect of this study is the use of data sets from the Global Atmospheric Research Program (GARP) Monsoon Experiment (MONEX) from a variety of observing platforms. These include winds from geostationary satellites, constant level balloons, dropwindsonde aircraft and an enhanced World Weather Watch network. The data sets were analyzed for a 46-day period from 16 May through 30 June 1979. A number of calculations were performed with this analysis. Of major interest is a finding that the kinetic energy of the zonal flow over the central Arabian Sea increases by an order of magnitude one week prior to the commencement of monsoon rain over central India. This study provides a MONEX time-averaged analysis for the low-level flow which is an update on the well-known Findlater analysis. A number of calculations show that the horizontal shear of the monsoon current provides substantial energy during the evolution of the onset vortex. The flow satisfies the necessary condition for the existence of instability. Corresponding stability diagrams exhibit substantial growth rates around the period of the formation of the onset vortex. The scale of maximum growth rate is closely in correspondence with the scale of the onset vortex. Finally, the conversion from zonal to eddy kinetic energy is demonstrated via a simple prediction experiment with the conservation of absolute vorticity as a constraint. A reasonable simulation of the onset vortex is shown in this experiment.
    publisherAmerican Meteorological Society
    titleOn the Onset Vortex of the Summer Monsoon
    typeJournal Paper
    journal volume109
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<0344:OTOVOT>2.0.CO;2
    journal fristpage344
    journal lastpage363
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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