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    A Hydrological Analysis of East Australian Floods Using Nimbus-5 Electrically Scanning Radiometer Data

    Source: Bulletin of the American Meteorological Society:;1979:;volume( 060 ):;issue: 012::page 1414
    Author:
    Allison, Lewis J.
    ,
    Schmugge, Thomas J.
    ,
    Byrne, Gavin
    DOI: 10.1175/1520-0477(1979)060<1414:AHAOEA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The chronological development and diminution of six floods in eastern Australia during January, February, and March 1974 were mapped for the first time by the Nimbus Electrically Scanning Microwave Radiometer (ESMR). Day and nighttime ESMR (19.35 GHz) coverage was analyzed for the low gradient, flooded Darling River system in New South Wales. Apparent movement of surface water as indicated by low brightness temperatures (<250 K, day and <240 K, night) was easily followed around the curved runoff basin along the northern shoreline of the flooded Darling River during this 3-month period. This pattern was in good agreement with flood crest data at selected river height gage stations, even under cloudy conditions.
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      A Hydrological Analysis of East Australian Floods Using Nimbus-5 Electrically Scanning Radiometer Data

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4160553
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    • Bulletin of the American Meteorological Society

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    contributor authorAllison, Lewis J.
    contributor authorSchmugge, Thomas J.
    contributor authorByrne, Gavin
    date accessioned2017-06-09T14:39:51Z
    date available2017-06-09T14:39:51Z
    date copyright1979/12/01
    date issued1979
    identifier issn0003-0007
    identifier otherams-23937.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160553
    description abstractThe chronological development and diminution of six floods in eastern Australia during January, February, and March 1974 were mapped for the first time by the Nimbus Electrically Scanning Microwave Radiometer (ESMR). Day and nighttime ESMR (19.35 GHz) coverage was analyzed for the low gradient, flooded Darling River system in New South Wales. Apparent movement of surface water as indicated by low brightness temperatures (<250 K, day and <240 K, night) was easily followed around the curved runoff basin along the northern shoreline of the flooded Darling River during this 3-month period. This pattern was in good agreement with flood crest data at selected river height gage stations, even under cloudy conditions.
    publisherAmerican Meteorological Society
    titleA Hydrological Analysis of East Australian Floods Using Nimbus-5 Electrically Scanning Radiometer Data
    typeJournal Paper
    journal volume60
    journal issue12
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1979)060<1414:AHAOEA>2.0.CO;2
    journal fristpage1414
    journal lastpage1427
    treeBulletin of the American Meteorological Society:;1979:;volume( 060 ):;issue: 012
    contenttypeFulltext
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