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    Monitoring Tropical Cyclone Evolution with NOAA Satellite Microwave Observations

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 005::page 714
    Author:
    Velden, Christopher S.
    ,
    Smith, William L.
    DOI: 10.1175/1520-0450(1983)022<0714:MTCEWN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: NOAA satellite microwave soundings, which penetrate high clouds, delineate the development and dissipation of the upper tropospheric warm core associated with a tropical cyclone. The storm's ?core? may be detected from microwave imagery. Vertical cross sections reveal the intensification of the upper tropospheric warm core as the storm developes, and the downward propagation of the warm core as the storm dissipates. Excellent correlation is found between the horizontal Laplacian of an upper tropospheric temperature field and the intensity of the storm, as categorized by its surface central pressure and maximum sustained wind speed at the eye wall. The microwave monitoring of tropical cyclones is achieved in real time at the University of Wisconsin's Space Science and Engineering Center through high-speed teleconnections to direct readout receiving systems at Wallops Island, Virginia and Redwood City, California.
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      Monitoring Tropical Cyclone Evolution with NOAA Satellite Microwave Observations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145615
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    • Journal of Climate and Applied Meteorology

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    contributor authorVelden, Christopher S.
    contributor authorSmith, William L.
    date accessioned2017-06-09T13:59:29Z
    date available2017-06-09T13:59:29Z
    date copyright1983/05/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10492.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145615
    description abstractNOAA satellite microwave soundings, which penetrate high clouds, delineate the development and dissipation of the upper tropospheric warm core associated with a tropical cyclone. The storm's ?core? may be detected from microwave imagery. Vertical cross sections reveal the intensification of the upper tropospheric warm core as the storm developes, and the downward propagation of the warm core as the storm dissipates. Excellent correlation is found between the horizontal Laplacian of an upper tropospheric temperature field and the intensity of the storm, as categorized by its surface central pressure and maximum sustained wind speed at the eye wall. The microwave monitoring of tropical cyclones is achieved in real time at the University of Wisconsin's Space Science and Engineering Center through high-speed teleconnections to direct readout receiving systems at Wallops Island, Virginia and Redwood City, California.
    publisherAmerican Meteorological Society
    titleMonitoring Tropical Cyclone Evolution with NOAA Satellite Microwave Observations
    typeJournal Paper
    journal volume22
    journal issue5
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<0714:MTCEWN>2.0.CO;2
    journal fristpage714
    journal lastpage724
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 005
    contenttypeFulltext
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