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contributor authorPicon, Laurence
contributor authorDesbois, Michel
date accessioned2017-06-09T15:12:20Z
date available2017-06-09T15:12:20Z
date copyright1990/08/01
date issued1990
identifier issn0894-8755
identifier otherams-3728.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4175378
description abstractMean monthly images from the water vapor channel of METEOSAT characteristically contain large-scale spatial structures, especially in tropical regions. The aim of this paper is to establish connections between these structures and large-scale circulation features. For this purpose, statistical relationships between radiances and some meteorological parameters provided by ECMWF analyses are studied. Temporal correlations are computed for two sizes of regions, in order to compare temporal changes associated with both large-scale circulations and smaller scale systems. The correlations obtained are poor, suggesting that the chosen parameters are not well related at short time scales. Temporal averages appear more suitable for these comparisons. As expected, the mean relative humidity yields the best correlation with the mean water vapor radiances. A (weaker) relationship exists also with mean dynamic fields: large water vapor radiances are almost always related to subsidence in the middle troposphere, divergence near the surface, and convergence in the upper troposphere. However, there is regional variability in the results., one explanation may be different contributions from horizontal advecion and vertical motions to the humidity of the middle troposphere.
publisherAmerican Meteorological Society
titleRelation between METEOSAT Water Vapor Radiance Fields and Large Scale Tropical Circulation Features
typeJournal Paper
journal volume3
journal issue8
journal titleJournal of Climate
identifier doi10.1175/1520-0442(1990)003<0865:RBMWVR>2.0.CO;2
journal fristpage865
journal lastpage876
treeJournal of Climate:;1990:;volume( 003 ):;issue: 008
contenttypeFulltext


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