A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds

Abstract The intensity of the Seasat altimeter return power over Antarctica varies in strong correlation with the intensity of model katabatic winds. It is also strongly correlated with the polarization of the passive microwave signal at 37 GHz of the Nimbus-7 SMMR data. It is shown that this is mos...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Remy, F., Minster, J. F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1991
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000042738
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042738
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author Remy, F.
Minster, J. F.
author_facet Remy, F.
Minster, J. F.
author_sort Remy, F.
collection Cambridge University Press
container_issue 125
container_start_page 3
container_title Journal of Glaciology
container_volume 37
description Abstract The intensity of the Seasat altimeter return power over Antarctica varies in strong correlation with the intensity of model katabatic winds. It is also strongly correlated with the polarization of the passive microwave signal at 37 GHz of the Nimbus-7 SMMR data. It is shown that this is most likely the result of the wind-induced micro-roughness of the ice surface.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Journal of Glaciology
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Journal of Glaciology
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
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language English
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op_doi https://doi.org/10.1017/s0022143000042738
op_source Journal of Glaciology
volume 37, issue 125, page 3-10
ISSN 0022-1430 1727-5652
publishDate 1991
publisher Cambridge University Press (CUP)
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spelling crcambridgeupr:10.1017/s0022143000042738 2025-01-16T19:31:45+00:00 A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds Remy, F. Minster, J. F. 1991 http://dx.doi.org/10.1017/s0022143000042738 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042738 en eng Cambridge University Press (CUP) Journal of Glaciology volume 37, issue 125, page 3-10 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1991 crcambridgeupr https://doi.org/10.1017/s0022143000042738 2024-02-08T08:40:23Z Abstract The intensity of the Seasat altimeter return power over Antarctica varies in strong correlation with the intensity of model katabatic winds. It is also strongly correlated with the polarization of the passive microwave signal at 37 GHz of the Nimbus-7 SMMR data. It is shown that this is most likely the result of the wind-induced micro-roughness of the ice surface. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Journal of Glaciology Cambridge University Press Antarctic The Antarctic Journal of Glaciology 37 125 3 10
spellingShingle Earth-Surface Processes
Remy, F.
Minster, J. F.
A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title_full A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title_fullStr A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title_full_unstemmed A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title_short A comparison between active and passive microwave measurements of the Antarctic ice sheet and their association with the surface katabatic winds
title_sort comparison between active and passive microwave measurements of the antarctic ice sheet and their association with the surface katabatic winds
topic Earth-Surface Processes
topic_facet Earth-Surface Processes
url http://dx.doi.org/10.1017/s0022143000042738
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000042738