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    The Infrared Horizon of the Planet Earth

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 002::page 73
    Author:
    Hanel, R. A.
    ,
    Bandeen, W. R.
    ,
    Conrath, B. J.
    DOI: 10.1175/1520-0469(1963)020<0073:TIHOTP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Horizon sensors are essential elements in the orientation systems of many space vehicles and satellites. Their design and an evaluation of their capabilities and limitations requires a knowledge of the spectral radiance emitted by the Earth. This report investigates the discontinuity between the surface, the atmosphere, and outer space for various latitudinal, seasonal, climatic, and meteorological conditions. Calculations are carried out for the following five spectral intervals?the water vapor band from 6.33 to 6.85 microns, the ozone band from 8.9 to 10.1 microns, the atmospheric window from 10.75 to 11.75 microns, the carbon dioxide band from 14 to 16 microns, and finally the rotational water vapor band from 21 to 125 microns. The superior properties of the carbon dioxide band and the rotational water vapor region for horizon sensor purposes are shown.
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      The Infrared Horizon of the Planet Earth

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150497
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    contributor authorHanel, R. A.
    contributor authorBandeen, W. R.
    contributor authorConrath, B. J.
    date accessioned2017-06-09T14:12:59Z
    date available2017-06-09T14:12:59Z
    date copyright1963/03/01
    date issued1963
    identifier issn0022-4928
    identifier otherams-14887.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150497
    description abstractHorizon sensors are essential elements in the orientation systems of many space vehicles and satellites. Their design and an evaluation of their capabilities and limitations requires a knowledge of the spectral radiance emitted by the Earth. This report investigates the discontinuity between the surface, the atmosphere, and outer space for various latitudinal, seasonal, climatic, and meteorological conditions. Calculations are carried out for the following five spectral intervals?the water vapor band from 6.33 to 6.85 microns, the ozone band from 8.9 to 10.1 microns, the atmospheric window from 10.75 to 11.75 microns, the carbon dioxide band from 14 to 16 microns, and finally the rotational water vapor band from 21 to 125 microns. The superior properties of the carbon dioxide band and the rotational water vapor region for horizon sensor purposes are shown.
    publisherAmerican Meteorological Society
    titleThe Infrared Horizon of the Planet Earth
    typeJournal Paper
    journal volume20
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1963)020<0073:TIHOTP>2.0.CO;2
    journal fristpage73
    journal lastpage86
    treeJournal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 002
    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
    yabeshDSpacePersian