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    An Intercomparison of Radiation Codes for Retrieving Upper–Tropospheric Humidity in the 6.3–mm Band: A Report from the First GVaP Workshop

    Source: Bulletin of the American Meteorological Society:;2000:;volume( 081 ):;issue: 004::page 797
    Author:
    Soden, B.
    ,
    Tjemkes, S.
    ,
    Schmetz, J.
    ,
    Saunders, R.
    ,
    Bates, J.
    ,
    Ellingson, B.
    ,
    Engelen, R.
    ,
    Garand, L.
    ,
    Jackson, D.
    ,
    Jedlovec, G.
    ,
    Kleespies, T.
    ,
    Randel, D.
    ,
    Rayer, P.
    ,
    Salathe, E.
    ,
    Schwarzkopf, D.
    ,
    Scott, N.
    ,
    Sohn, B.
    ,
    de Souza-Machado, S.
    ,
    Strow, L.
    ,
    Tobin, D.
    ,
    Turner, D.
    ,
    van Delst, P.
    ,
    Wehr, T.
    DOI: 10.1175/1520-0477(2000)081<0797:AIORCF>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: An intercomparison of radiation codes used in retrieving upper?tropospheric humidity (UTH) from observations in the n2 (6.3 mm) water vapor absorption band was performed. This intercomparison is one part of a coordinated effort within the Global Energy and Water Cycle Experiment Water Vapor Project to assess our ability to monitor the distribution and variations of upper?tropospheric moisture from spaceborne sensors. A total of 23 different codes, ranging from detailed line?by?line (LBL) models, to coarser?resolution narrowband (NB) models, to highly parameterized single?band (SB) models participated in the study. Forward calculations were performed using a carefully selected set of temperature and moisture profiles chosen to be representative of a wide range of atmospheric conditions. The LBL model calculations exhibited the greatest consistency with each other, typically agreeing to within 0.5 K in terms of the equivalent blackbody brightness temperature(Tb). The majority of NB and SB models agreed to within±1 K of the LBL models, although a few older models exhibited systematicTb biases in excess of 2 K. A discussion of the discrepancies between various models, their association with differences in model physics (e.g., continuum absorption), and their implications for UTH retrieval and radiance assimilation is presented.
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      An Intercomparison of Radiation Codes for Retrieving Upper–Tropospheric Humidity in the 6.3–mm Band: A Report from the First GVaP Workshop

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4161692
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    • Bulletin of the American Meteorological Society

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    contributor authorSoden, B.
    contributor authorTjemkes, S.
    contributor authorSchmetz, J.
    contributor authorSaunders, R.
    contributor authorBates, J.
    contributor authorEllingson, B.
    contributor authorEngelen, R.
    contributor authorGarand, L.
    contributor authorJackson, D.
    contributor authorJedlovec, G.
    contributor authorKleespies, T.
    contributor authorRandel, D.
    contributor authorRayer, P.
    contributor authorSalathe, E.
    contributor authorSchwarzkopf, D.
    contributor authorScott, N.
    contributor authorSohn, B.
    contributor authorde Souza-Machado, S.
    contributor authorStrow, L.
    contributor authorTobin, D.
    contributor authorTurner, D.
    contributor authorvan Delst, P.
    contributor authorWehr, T.
    date accessioned2017-06-09T14:42:38Z
    date available2017-06-09T14:42:38Z
    date copyright2000/04/01
    date issued2000
    identifier issn0003-0007
    identifier otherams-24962.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161692
    description abstractAn intercomparison of radiation codes used in retrieving upper?tropospheric humidity (UTH) from observations in the n2 (6.3 mm) water vapor absorption band was performed. This intercomparison is one part of a coordinated effort within the Global Energy and Water Cycle Experiment Water Vapor Project to assess our ability to monitor the distribution and variations of upper?tropospheric moisture from spaceborne sensors. A total of 23 different codes, ranging from detailed line?by?line (LBL) models, to coarser?resolution narrowband (NB) models, to highly parameterized single?band (SB) models participated in the study. Forward calculations were performed using a carefully selected set of temperature and moisture profiles chosen to be representative of a wide range of atmospheric conditions. The LBL model calculations exhibited the greatest consistency with each other, typically agreeing to within 0.5 K in terms of the equivalent blackbody brightness temperature(Tb). The majority of NB and SB models agreed to within±1 K of the LBL models, although a few older models exhibited systematicTb biases in excess of 2 K. A discussion of the discrepancies between various models, their association with differences in model physics (e.g., continuum absorption), and their implications for UTH retrieval and radiance assimilation is presented.
    publisherAmerican Meteorological Society
    titleAn Intercomparison of Radiation Codes for Retrieving Upper–Tropospheric Humidity in the 6.3–mm Band: A Report from the First GVaP Workshop
    typeJournal Paper
    journal volume81
    journal issue4
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(2000)081<0797:AIORCF>2.3.CO;2
    journal fristpage797
    journal lastpage808
    treeBulletin of the American Meteorological Society:;2000:;volume( 081 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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