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    Observations of Thermal and Precipitation Structure in a Tropical Cyclone by Means of Passive Microwave Imagery near 118 GHZ

    Source: Journal of Applied Meteorology:;1996:;volume( 035 ):;issue: 005::page 671
    Author:
    Schwartz, M. J.
    ,
    Barrett, J. W.
    ,
    Fieguth, P. W.
    ,
    Rosenkranz, P. W.
    ,
    Spina, M. S.
    ,
    Staelin, D. H.
    DOI: 10.1175/1520-0450(1996)035<0671:OOTAPS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An imaging microwave radiometer with eight double-sideband channels centered on the 118-GHz oxygen resonance was flown on a high-altitude aircraft over a tropical cyclone in the Coral Sea. The measurements clearly resolved an eyewall of strong convection and a warm core within the eye. Brightness temperatures observed within the eye were approximately 10 K warmer than those observed in clear air 100 km or more away. This warming extended somewhat beyond the eyewall in the highest (most opaque) channel. The temperature profile in the eye, central pressure, and convective cell-top altitudes are inferred from the data.
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      Observations of Thermal and Precipitation Structure in a Tropical Cyclone by Means of Passive Microwave Imagery near 118 GHZ

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4147632
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    • Journal of Applied Meteorology

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    contributor authorSchwartz, M. J.
    contributor authorBarrett, J. W.
    contributor authorFieguth, P. W.
    contributor authorRosenkranz, P. W.
    contributor authorSpina, M. S.
    contributor authorStaelin, D. H.
    date accessioned2017-06-09T14:05:42Z
    date available2017-06-09T14:05:42Z
    date copyright1996/05/01
    date issued1996
    identifier issn0894-8763
    identifier otherams-12307.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147632
    description abstractAn imaging microwave radiometer with eight double-sideband channels centered on the 118-GHz oxygen resonance was flown on a high-altitude aircraft over a tropical cyclone in the Coral Sea. The measurements clearly resolved an eyewall of strong convection and a warm core within the eye. Brightness temperatures observed within the eye were approximately 10 K warmer than those observed in clear air 100 km or more away. This warming extended somewhat beyond the eyewall in the highest (most opaque) channel. The temperature profile in the eye, central pressure, and convective cell-top altitudes are inferred from the data.
    publisherAmerican Meteorological Society
    titleObservations of Thermal and Precipitation Structure in a Tropical Cyclone by Means of Passive Microwave Imagery near 118 GHZ
    typeJournal Paper
    journal volume35
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1996)035<0671:OOTAPS>2.0.CO;2
    journal fristpage671
    journal lastpage678
    treeJournal of Applied Meteorology:;1996:;volume( 035 ):;issue: 005
    contenttypeFulltext
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