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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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