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contributor authorDeb, S. K.
contributor authorKishtawal, C. M.
contributor authorPal, P. K.
contributor authorJoshi, P. C.
date accessioned2017-06-09T16:22:27Z
date available2017-06-09T16:22:27Z
date copyright2008/12/01
date issued2008
identifier issn1558-8424
identifier otherams-66686.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208049
description abstractThe remotely sensed upper-tropospheric water vapor wind information has been of increasing interest for operational meteorology. A new tracer selection based on a local image anomaly and tracking procedure, itself based on Nash?Sutcliffe model efficiency, is demonstrated here for the estimation of upper-tropospheric water vapor winds both for cloudy and cloud-free regions from water vapor images. The pressure height of the selected water vapor tracers is calculated empirically using a height assignment technique based on a genetic algorithm. The new technique shows encouraging results when compared with Meteosat-5 water vapor winds over the Indian Ocean region. The water vapor winds produced by the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) from Meteosat-5 and the present algorithm are compared with collocated radiosonde observations according to Coordination Group for Meteorological Satellites guidelines. The proposed algorithm shows better accuracy in terms of mean vector difference, rms vector difference, standard deviation, speed bias, number of collocations, and mean speed and mean direction differences. Also it is found that the sensitivity of the spatial consistency check in the quality indicator is not so significant for the improvement of statistics.
publisherAmerican Meteorological Society
titleA Modified Tracer Selection and Tracking Procedure to Derive Winds Using Water Vapor Imagers
typeJournal Paper
journal volume47
journal issue12
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/2008JAMC1925.1
journal fristpage3252
journal lastpage3263
treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 012
contenttypeFulltext


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