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    Atmospheric Sounding Near 118 GHz

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 010::page 1234
    Author:
    Ali, Ali D. S.
    ,
    Rosenkranz, Philip W.
    ,
    Staelin, David H.
    DOI: 10.1175/1520-0450(1980)019<1234:ASNG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The thermal emission spectrum of the atmosphere near the 118 GHz oxygen resonance has been measured from the NASA Convair-990 aircraft as it flew over clear air and storms. The instrument viewed the ground 45° from nadir with a 7.5° beamwidth. Brightness temperatures were measured in six bands 200 MHz wide centered at frequencies 821?1891 MHz from the line at 118.7505 GHz. The double-sideband super-heterodyne receiver had ?1 K sensitivity for 1 s integration. Comparison of observed clear air brightness temperatures (from 238 mb) with those computed for a coincident dropsonde yielded agreement within 1.4 K; the retrieved temperature profile agreed with the dropsonde with an average magnitude error of 1.4 K. Observations over precipitation yielded brightness perturbations as large as 30 K.
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      Atmospheric Sounding Near 118 GHz

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4233525
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    contributor authorAli, Ali D. S.
    contributor authorRosenkranz, Philip W.
    contributor authorStaelin, David H.
    date accessioned2017-06-09T17:40:39Z
    date available2017-06-09T17:40:39Z
    date copyright1980/10/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9978.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233525
    description abstractThe thermal emission spectrum of the atmosphere near the 118 GHz oxygen resonance has been measured from the NASA Convair-990 aircraft as it flew over clear air and storms. The instrument viewed the ground 45° from nadir with a 7.5° beamwidth. Brightness temperatures were measured in six bands 200 MHz wide centered at frequencies 821?1891 MHz from the line at 118.7505 GHz. The double-sideband super-heterodyne receiver had ?1 K sensitivity for 1 s integration. Comparison of observed clear air brightness temperatures (from 238 mb) with those computed for a coincident dropsonde yielded agreement within 1.4 K; the retrieved temperature profile agreed with the dropsonde with an average magnitude error of 1.4 K. Observations over precipitation yielded brightness perturbations as large as 30 K.
    publisherAmerican Meteorological Society
    titleAtmospheric Sounding Near 118 GHz
    typeJournal Paper
    journal volume19
    journal issue10
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1980)019<1234:ASNG>2.0.CO;2
    journal fristpage1234
    journal lastpage1238
    treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 010
    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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