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contributor authorMcMurdie, Lynn A.
contributor authorLevy, Gad
contributor authorKatsaros, Kristina B.
date accessioned2017-06-09T16:06:20Z
date available2017-06-09T16:06:20Z
date copyright1987/07/01
date issued1987
identifier issn0027-0644
identifier otherams-61036.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201773
description abstractFields of divergence calculated from the Seasat-A Satellite Scatterometer winds and fields of integrated water vapor and rainrate from the Scanning Multichannel Microwave Radiometer on Seasat are constructed for three different midlatitude cyclones. These storms include an explosively deepening cyclone that occurred in the North Atlantic (also known as the Queen Elizabeth II cyclone), a storm that occurred in the North Pacific, and a Southern Ocean storm. In all three cases, the regions of convergence and atmospheric water (vapor and rain) are consistent with each other and help to define features of each storm. The vertical distribution of moisture is inferred for one case using both the convergence pattern and the integrated water vapor field. In another, interpretation of the convergence field in a data gap region is aided by the water vapor field. In all three cases, surface low pressure centers, fronts, and even frontal waves are clearly evident as areas of convergence, and increased water vapor and rainrate.
publisherAmerican Meteorological Society
titleOn the Relationship Between Scatterometer-Derived Convergences and Atmospheric Moisture
typeJournal Paper
journal volume115
journal issue7
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1987)115<1281:OTRBSD>2.0.CO;2
journal fristpage1281
journal lastpage1294
treeMonthly Weather Review:;1987:;volume( 115 ):;issue: 007
contenttypeFulltext


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