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    Validation of the Upper Tropospheric Relative Humidity Determined from METEOSAT Data

    Source: Journal of Atmospheric and Oceanic Technology:;1989:;volume( 006 ):;issue: 002::page 359
    Author:
    Turpeinen, Olli M.
    ,
    Schmetz, Johannes
    DOI: 10.1175/1520-0426(1989)006<0359:VOTUTR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The purpose of this note is to ?validate? the upper tropospheric humidity (UTH) operationally extracted from the 6.3 ?m channel data of METEOSAT. The validation is carded out by comparing the satellite data with observed humidifies from the conventional network of radiosondes. The validation is not an absolute error assessment of the UTH, but rather an intercomparison, because the upper-tropospheric radiosonde humidities may not be very accurate. The results for three latitude belts indicate that the estimated humidity in the upper troposphere shows a fairly high linear correlation (coefficients 0.64?0.89) with the observed humidity and that the slope of the regression line ranges from 0.82?0.89. The rms-error of the UTH is generally less than 10%. The UTH tends to underestimate the observed humidity by about 4%. This relative bias is most pronounced in the midlatitude belts.
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      Validation of the Upper Tropospheric Relative Humidity Determined from METEOSAT Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4186289
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    contributor authorTurpeinen, Olli M.
    contributor authorSchmetz, Johannes
    date accessioned2017-06-09T15:33:38Z
    date available2017-06-09T15:33:38Z
    date copyright1989/04/01
    date issued1989
    identifier issn0739-0572
    identifier otherams-471.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4186289
    description abstractThe purpose of this note is to ?validate? the upper tropospheric humidity (UTH) operationally extracted from the 6.3 ?m channel data of METEOSAT. The validation is carded out by comparing the satellite data with observed humidifies from the conventional network of radiosondes. The validation is not an absolute error assessment of the UTH, but rather an intercomparison, because the upper-tropospheric radiosonde humidities may not be very accurate. The results for three latitude belts indicate that the estimated humidity in the upper troposphere shows a fairly high linear correlation (coefficients 0.64?0.89) with the observed humidity and that the slope of the regression line ranges from 0.82?0.89. The rms-error of the UTH is generally less than 10%. The UTH tends to underestimate the observed humidity by about 4%. This relative bias is most pronounced in the midlatitude belts.
    publisherAmerican Meteorological Society
    titleValidation of the Upper Tropospheric Relative Humidity Determined from METEOSAT Data
    typeJournal Paper
    journal volume6
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1989)006<0359:VOTUTR>2.0.CO;2
    journal fristpage359
    journal lastpage364
    treeJournal of Atmospheric and Oceanic Technology:;1989:;volume( 006 ):;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
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