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contributor authorVandemark, Douglas
contributor authorEdson, James B.
contributor authorChapron, Bertrand
date accessioned2017-06-09T14:07:25Z
date available2017-06-09T14:07:25Z
date copyright1997/06/01
date issued1997
identifier issn0739-0572
identifier otherams-1285.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148234
description abstractAircraft altimeter and in situ measurements are used to examine relationships between altimeter backscatter and the magnitude of near-surface wind and friction velocities. Comparison of altimeter radar cross section with wind speed is made through the modified Chelton?Wentz algorithm. Improved agreement is found after correcting 10-m winds for both surface current and atmospheric stability. An altimeter friction velocity algorithm is derived based on the wind speed model and an open-ocean drag coefficient. Close agreement between altimeter- and in situ?derived friction velocities is found. For this dataset, quality of the altimeter inversion to surface friction velocity is comparable to that for adjusted winds and clearly better than the inversion to true 10-m wind speed.
publisherAmerican Meteorological Society
titleAltimeter Estimation of Sea Surface Wind Stress for Light to Moderate Winds
typeJournal Paper
journal volume14
journal issue3
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/1520-0426(1997)014<0716:AEOSSW>2.0.CO;2
journal fristpage716
journal lastpage722
treeJournal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 003
contenttypeFulltext


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