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contributor authorWalsh, E. J.
contributor authorWright, C. W.
contributor authorBanner, M. L.
contributor authorVandemark, D. C.
contributor authorChapron, B.
contributor authorJensen, J.
contributor authorLee, S.
date accessioned2017-06-09T16:20:20Z
date available2017-06-09T16:20:20Z
date copyright2008/03/01
date issued2008
identifier issn0022-3670
identifier otherams-66030.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207321
description abstractDuring the Southern Ocean Waves Experiment (SOWEX), registered ocean wave topography and backscattered power data at Ka band (36 GHz) were collected with the NASA Scanning Radar Altimeter (SRA) off the coast of Tasmania under a wide range of wind and sea conditions, from quiescent to gale-force winds with 9-m significant wave height. Collection altitude varied from 35 m to over 1 km, allowing determination of the sea surface mean square slope (mss), the directional wave spectrum, and the detailed variation of backscattered power with incidence angle, which deviated from a simple Gaussian scattering model. The non-Gaussian characteristics of the backscatter increased systematically with the mss, suggesting that a global model to characterize Ka-band radar backscatter from the sea surface within 25° of nadir might be possible.
publisherAmerican Meteorological Society
titleThe Southern Ocean Waves Experiment. Part III: Sea Surface Slope Statistics and Near-Nadir Remote Sensing
typeJournal Paper
journal volume38
journal issue3
journal titleJournal of Physical Oceanography
identifier doi10.1175/2007JPO3771.1
journal fristpage670
journal lastpage685
treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 003
contenttypeFulltext


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