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    Resolution of the Nimbus High Resolution Infrared Radiometer

    Source: Journal of Applied Meteorology:;1965:;volume( 004 ):;issue: 004::page 492
    Author:
    Fujita, Tetsuya
    ,
    Bandeen, William
    DOI: 10.1175/1520-0450(1965)004<0492:ROTNHR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: For the purpose of evaluating the resolution of the High Resolution Infrared Radiometer (HRIR) flown on board the Nimbus I meteorological satellite, three cloud-free regions in the western United States?the Grand Canyon, Death Valley, and Sierra Nevada?were selected. Enlarged HRIR pictures and the analog frequency traces of the scan lines in the pictures were examined in an attempt to investigate the types of noise superimposed on the signals. Two types of noise which appear in periodic and oscillatory fashions were found. The latter can be eliminated by taking running-mean values at one-degree scan angle intervals. The equivalent blackbody temperatures thus obtained were analysed over these three regions, leading to the determination of the apparent temperature lapse rate inside the Grand Canyon atmosphere and of the temperature of Lake Tahoe and other lakes in the Sierra Nevadas. Death Valley was found to be about 10C warmer than the surrounding desert area 5000 ft high. An attempt was also made to produce an HRIR picture with isoneph contours similar to the iso-echo presentation of radar pictures.
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      Resolution of the Nimbus High Resolution Infrared Radiometer

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4214378
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    contributor authorFujita, Tetsuya
    contributor authorBandeen, William
    date accessioned2017-06-09T16:41:43Z
    date available2017-06-09T16:41:43Z
    date copyright1965/08/01
    date issued1965
    identifier issn0021-8952
    identifier otherams-7238.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214378
    description abstractFor the purpose of evaluating the resolution of the High Resolution Infrared Radiometer (HRIR) flown on board the Nimbus I meteorological satellite, three cloud-free regions in the western United States?the Grand Canyon, Death Valley, and Sierra Nevada?were selected. Enlarged HRIR pictures and the analog frequency traces of the scan lines in the pictures were examined in an attempt to investigate the types of noise superimposed on the signals. Two types of noise which appear in periodic and oscillatory fashions were found. The latter can be eliminated by taking running-mean values at one-degree scan angle intervals. The equivalent blackbody temperatures thus obtained were analysed over these three regions, leading to the determination of the apparent temperature lapse rate inside the Grand Canyon atmosphere and of the temperature of Lake Tahoe and other lakes in the Sierra Nevadas. Death Valley was found to be about 10C warmer than the surrounding desert area 5000 ft high. An attempt was also made to produce an HRIR picture with isoneph contours similar to the iso-echo presentation of radar pictures.
    publisherAmerican Meteorological Society
    titleResolution of the Nimbus High Resolution Infrared Radiometer
    typeJournal Paper
    journal volume4
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1965)004<0492:ROTNHR>2.0.CO;2
    journal fristpage492
    journal lastpage503
    treeJournal of Applied Meteorology:;1965:;volume( 004 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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