On the azimuthally anisotropy effects of polarization for altimetric measurements

Abstract—We have investigated the effect of the radar-altimeter antenna polarization on European Remote-sensing Satellite and Envisat observations of the media penetrable by a radar mi-crowave such as ice sheets. This effect is due to the complex interaction between the radar wave, the subsurface ba...

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Main Authors: Frédérique Rémy, Benoît Legrésy, Jérôme Benveniste
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.9405
http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.570.9405 2023-05-15T13:42:36+02:00 On the azimuthally anisotropy effects of polarization for altimetric measurements Frédérique Rémy Benoît Legrésy Jérôme Benveniste The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.9405 http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.9405 http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf text ftciteseerx 2016-01-08T12:31:48Z Abstract—We have investigated the effect of the radar-altimeter antenna polarization on European Remote-sensing Satellite and Envisat observations of the media penetrable by a radar mi-crowave such as ice sheets. This effect is due to the complex interaction between the radar wave, the subsurface backscatter, and the antenna polarization direction. It is modulated by the angle between the antenna polarization and the direction of the anisotropy of the target. Thus, it depends on both the anisotropy direction and the interaction between the radar wave and the reflecting surface. This effect leads to one of the most complex and least understood errors of radar altimetry over ice sheets and can be clearly identified when looking at the crossover differences between ascending and descending satellite tracks. The crossover differences are as large as a few decibels for a backscattering co-efficient and a few meters for height, and affect more strongly the Ku-band than the S-band. This causes limitations and difficulties for the processing of altimetric observations, for instance when comparing time series from different satellites whose polarization geometry differs. This will be the case when a new altimeter will fly on a different orbit, as planned for CryoSat. Nevertheless, the ability of both the roughness anisotropy direction and the subsurface modulation to be inverted with satisfactory precision by using simultaneous observations at crossover points between two different satellites is demonstrated here. Thus, it offers a unique way of describing this error accurately to correct for it. Index Terms—Altimetry, Antarctica, ice sheet. I. Text Antarc* Antarctica Ice Sheet Unknown
institution Open Polar
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op_collection_id ftciteseerx
language English
description Abstract—We have investigated the effect of the radar-altimeter antenna polarization on European Remote-sensing Satellite and Envisat observations of the media penetrable by a radar mi-crowave such as ice sheets. This effect is due to the complex interaction between the radar wave, the subsurface backscatter, and the antenna polarization direction. It is modulated by the angle between the antenna polarization and the direction of the anisotropy of the target. Thus, it depends on both the anisotropy direction and the interaction between the radar wave and the reflecting surface. This effect leads to one of the most complex and least understood errors of radar altimetry over ice sheets and can be clearly identified when looking at the crossover differences between ascending and descending satellite tracks. The crossover differences are as large as a few decibels for a backscattering co-efficient and a few meters for height, and affect more strongly the Ku-band than the S-band. This causes limitations and difficulties for the processing of altimetric observations, for instance when comparing time series from different satellites whose polarization geometry differs. This will be the case when a new altimeter will fly on a different orbit, as planned for CryoSat. Nevertheless, the ability of both the roughness anisotropy direction and the subsurface modulation to be inverted with satisfactory precision by using simultaneous observations at crossover points between two different satellites is demonstrated here. Thus, it offers a unique way of describing this error accurately to correct for it. Index Terms—Altimetry, Antarctica, ice sheet. I.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Frédérique Rémy
Benoît Legrésy
Jérôme Benveniste
spellingShingle Frédérique Rémy
Benoît Legrésy
Jérôme Benveniste
On the azimuthally anisotropy effects of polarization for altimetric measurements
author_facet Frédérique Rémy
Benoît Legrésy
Jérôme Benveniste
author_sort Frédérique Rémy
title On the azimuthally anisotropy effects of polarization for altimetric measurements
title_short On the azimuthally anisotropy effects of polarization for altimetric measurements
title_full On the azimuthally anisotropy effects of polarization for altimetric measurements
title_fullStr On the azimuthally anisotropy effects of polarization for altimetric measurements
title_full_unstemmed On the azimuthally anisotropy effects of polarization for altimetric measurements
title_sort on the azimuthally anisotropy effects of polarization for altimetric measurements
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.9405
http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf
genre Antarc*
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctica
Ice Sheet
op_source http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf
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http://etienne.berthier.free.fr/ftp/51-Remy-anisotropy-2006.pdf
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