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contributor authorLiou, K. N.
contributor authorOu, S. C.
contributor authorTakano, Y.
contributor authorLiu, Q.
date accessioned2017-06-09T16:52:18Z
date available2017-06-09T16:52:18Z
date copyright2005/07/01
date issued2005
identifier issn0022-4928
identifier otherams-75663.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218024
description abstractThe delta-four-stream polarized (vector) thermal radiative transfer has been formulated and numerically tested specifically for application to satellite data assimilation in cloudy atmospheres. It is shown that for thermal emission in the earth?s atmosphere, the [I, Q] component of the Stokes vector can be decoupled from the [U, V] component and that the solution of the vector equation set involving the four-stream approximation can be expressed in an analytic form similar to the scalar case. Thus, the computer time requirement can be optimized for the simulation of forward radiances and their derivatives. Computations have been carried out to illustrate the accuracy and efficiency of this method by comparing radiance and polarization results to those computed from the exact doubling method for radiative transfer for a number of thermal infrared and microwave frequencies. Excellent agreement within 1% is shown for the radiance results for all satellite viewing angles and cloud optical depths. For polarization, differences between the two are less than 5% if brightness temperature is used in the analysis. On balance of the computational speed and accuracy, the four-stream approximation for radiative transfer appears to be an attractive means for the simulation of cloudy radiances and polarization for research and data assimilation purposes.
publisherAmerican Meteorological Society
titleA Polarized Delta-Four-Stream Approximation for Infrared and Microwave Radiative Transfer: Part I
typeJournal Paper
journal volume62
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS3476.1
journal fristpage2542
journal lastpage2554
treeJournal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 007
contenttypeFulltext


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