A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal
We have examined the characteristics of the GPS signal reflected off the sea ice surface and collected by an airborne or spaceborne receiver, forming a bistatic radar. The constellation of existing transmitters allows gathering bistatic reflections off the sea ice surface at different incidence angl...
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ftnasajpl:oai:trs.jpl.nasa.gov:2014/10988 2023-05-15T18:16:51+02:00 A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal Zuffada, C. Zavorotny, V. 2004-09-17T19:44:25Z 2600859 bytes application/pdf http://hdl.handle.net/2014/10988 en_US eng Fall Meeting 2002 San Francisco, CA, USA 02-2891 http://hdl.handle.net/2014/10988 GPS ice thickness rough surface scattering 2004 ftnasajpl 2021-12-23T13:15:40Z We have examined the characteristics of the GPS signal reflected off the sea ice surface and collected by an airborne or spaceborne receiver, forming a bistatic radar. The constellation of existing transmitters allows gathering bistatic reflections off the sea ice surface at different incidence angles over the course of a day, in contrast to a traditional radar that measures backscattering. We expect to see a strong coherent signal which is much higher than the incoherent one because of forward reflections from very smooth (particularly at L-band) and highly saline first year ice. Other/Unknown Material Sea ice JPL Technical Report Server |
institution |
Open Polar |
collection |
JPL Technical Report Server |
op_collection_id |
ftnasajpl |
language |
English |
topic |
GPS ice thickness rough surface scattering |
spellingShingle |
GPS ice thickness rough surface scattering Zuffada, C. Zavorotny, V. A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
topic_facet |
GPS ice thickness rough surface scattering |
description |
We have examined the characteristics of the GPS signal reflected off the sea ice surface and collected by an airborne or spaceborne receiver, forming a bistatic radar. The constellation of existing transmitters allows gathering bistatic reflections off the sea ice surface at different incidence angles over the course of a day, in contrast to a traditional radar that measures backscattering. We expect to see a strong coherent signal which is much higher than the incoherent one because of forward reflections from very smooth (particularly at L-band) and highly saline first year ice. |
author |
Zuffada, C. Zavorotny, V. |
author_facet |
Zuffada, C. Zavorotny, V. |
author_sort |
Zuffada, C. |
title |
A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
title_short |
A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
title_full |
A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
title_fullStr |
A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
title_full_unstemmed |
A novel technique for characterizing the thickness of first-year sea ice with the GPS reflected signal |
title_sort |
novel technique for characterizing the thickness of first-year sea ice with the gps reflected signal |
publishDate |
2004 |
url |
http://hdl.handle.net/2014/10988 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
Fall Meeting 2002 San Francisco, CA, USA 02-2891 http://hdl.handle.net/2014/10988 |
_version_ |
1766190767889448960 |