Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections

The authors report the first results in studying the polarization anisotropy of themicrowave backscatter from nadir observations provided by Jason-1 altimeter in both Ku-and C-band. A small but clear wind direction signal for wind speeds above 6 m/s is revealed.These azimuthal variations of radar cr...

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Main Authors: Bertrand Chapron, Ngan Tran
Format: Article
Language:English
Published: MDPI AG 2006-03-01
Series:Sensors
Subjects:
Online Access:http://www.mdpi.com/1424-8220/6/3/193/
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author Bertrand Chapron
Ngan Tran
author_facet Bertrand Chapron
Ngan Tran
author_sort Bertrand Chapron
collection DOAJ
description The authors report the first results in studying the polarization anisotropy of themicrowave backscatter from nadir observations provided by Jason-1 altimeter in both Ku-and C-band. A small but clear wind direction signal for wind speeds above 6 m/s is revealed.These azimuthal variations of radar cross-section increase with increasing wind speed up to14 m/s. The signatures then level off at higher winds. These results extend, for the first time,recent theoretical improved scattering approximation, and point some similarities betweenscattering and emission mechanisms at nadir. The observed directional effect can thus beinterpreted as a signature of the curvature anisotropy of wind-generated short-scale waves.Sensitivities to both wind speed and sea state are also reported in the present analysis.
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spelling doaj.art-b72c7eb69cce4b78b142d7a5a4da2d9d2022-12-22T03:58:32ZengMDPI AGSensors1424-82202006-03-016319320710.3390/s6030193Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-SectionsBertrand ChapronNgan TranThe authors report the first results in studying the polarization anisotropy of themicrowave backscatter from nadir observations provided by Jason-1 altimeter in both Ku-and C-band. A small but clear wind direction signal for wind speeds above 6 m/s is revealed.These azimuthal variations of radar cross-section increase with increasing wind speed up to14 m/s. The signatures then level off at higher winds. These results extend, for the first time,recent theoretical improved scattering approximation, and point some similarities betweenscattering and emission mechanisms at nadir. The observed directional effect can thus beinterpreted as a signature of the curvature anisotropy of wind-generated short-scale waves.Sensitivities to both wind speed and sea state are also reported in the present analysis.http://www.mdpi.com/1424-8220/6/3/193/Altimeterradar cross sectionpolarizationwind directionsea state.
spellingShingle Bertrand Chapron
Ngan Tran
Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
Sensors
Altimeter
radar cross section
polarization
wind direction
sea state.
title Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
title_full Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
title_fullStr Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
title_full_unstemmed Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
title_short Combined Wind Vector and Sea State Impact on Ocean Nadir-Viewing Ku- and C-Band Radar Cross-Sections
title_sort combined wind vector and sea state impact on ocean nadir viewing ku and c band radar cross sections
topic Altimeter
radar cross section
polarization
wind direction
sea state.
url http://www.mdpi.com/1424-8220/6/3/193/
work_keys_str_mv AT bertrandchapron combinedwindvectorandseastateimpactonoceannadirviewingkuandcbandradarcrosssections
AT ngantran combinedwindvectorandseastateimpactonoceannadirviewingkuandcbandradarcrosssections