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    Stratospheric Temperature Profiles from Limb Radiance Measurements

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 005::page 867
    Author:
    McKee, Thomas B.
    ,
    Cox, Stephen K.
    DOI: 10.1175/1520-0450(1973)012<0867:STPFLR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Stlratospheric temperature profiles have been inferred from limb radiance data. The limb radiance observations were made from an Aerobee rocket flown on 7 February 1970 from White Sands Missile Range, N.M. The inferred temperatures were similar to those available from rocket sounding data. Horizontal variations of temperature at the 10-mb surface agreed with radiosonde data; however, the inferred temperatures were systematically warmer at 10 mb with larger increases of temperature from 30 to 10 nab than comparative radiosonde data. Two of the inferred temperature profiles provide an excellent example in which two measurements are sufficiently alike to separate real vertical temperature structure from effects of random radiance noise. Vertical resolution was about 2 km and the largest lapse noted was near dry adiabatic.
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      Stratospheric Temperature Profiles from Limb Radiance Measurements

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4229455
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    contributor authorMcKee, Thomas B.
    contributor authorCox, Stephen K.
    date accessioned2017-06-09T17:28:34Z
    date available2017-06-09T17:28:34Z
    date copyright1973/08/01
    date issued1973
    identifier issn0021-8952
    identifier otherams-8595.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229455
    description abstractStlratospheric temperature profiles have been inferred from limb radiance data. The limb radiance observations were made from an Aerobee rocket flown on 7 February 1970 from White Sands Missile Range, N.M. The inferred temperatures were similar to those available from rocket sounding data. Horizontal variations of temperature at the 10-mb surface agreed with radiosonde data; however, the inferred temperatures were systematically warmer at 10 mb with larger increases of temperature from 30 to 10 nab than comparative radiosonde data. Two of the inferred temperature profiles provide an excellent example in which two measurements are sufficiently alike to separate real vertical temperature structure from effects of random radiance noise. Vertical resolution was about 2 km and the largest lapse noted was near dry adiabatic.
    publisherAmerican Meteorological Society
    titleStratospheric Temperature Profiles from Limb Radiance Measurements
    typeJournal Paper
    journal volume12
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1973)012<0867:STPFLR>2.0.CO;2
    journal fristpage867
    journal lastpage873
    treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 005
    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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