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contributor authorPatoux, Jérôme
contributor authorBrown, Robert A.
date accessioned2017-06-09T14:08:19Z
date available2017-06-09T14:08:19Z
date copyright2002/02/01
date issued2002
identifier issn0894-8763
identifier otherams-13116.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148531
description abstractGiven a field of geostrophic winds and at least one pressure observation, a pressure field can be computed. If the winds are in reality gradient winds, then a correction must be applied to calculate the actual geostrophic winds. Here a method is proposed for including a gradient wind correction in the retrieval of geostrophic winds from Quick Scatterometer (QuikSCAT) surface measurements with a planetary boundary layer model. This correction translates into a better estimate of the corresponding surface pressure fields. The scheme is assessed by comparing these pressure fields to buoy measurements in the Gulf of Alaska and to radiosonde measurements in Hurricane Floyd. The gradient wind correction has a curvature component and a time-dependent component. Their relative magnitude is evaluated.
publisherAmerican Meteorological Society
titleA Gradient Wind Correction for Surface Pressure Fields Retrieved from Scatterometer Winds
typeJournal Paper
journal volume41
journal issue2
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(2002)041<0133:AGWCFS>2.0.CO;2
journal fristpage133
journal lastpage143
treeJournal of Applied Meteorology:;2002:;volume( 041 ):;issue: 002
contenttypeFulltext


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