with the snow surface. The backscatter coefficient of the surface is derived using the IEM method [Fung, A. K. (1994). Microwave scattering and emission models and their applications, Boston, MA: Artech House.]. The sub-surface signal takes into account both the layering effects and the

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Altimeter
Antarctic ice sheet
Snowpack properties
Snow compaction
Radar modelling
Antarctic
Antarc*
Ice Sheet
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.2769
http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.595.2769
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.595.2769 2023-05-15T13:46:54+02:00 The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.2769 http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.2769 http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf Altimeter Antarctic ice sheet Snowpack properties Snow compaction Radar modelling text 2007 ftciteseerx 2016-01-08T13:42:16Z with the snow surface. The backscatter coefficient of the surface is derived using the IEM method [Fung, A. K. (1994). Microwave scattering and emission models and their applications, Boston, MA: Artech House.]. The sub-surface signal takes into account both the layering effects and the Text Antarc* Antarctic Ice Sheet Unknown Antarctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Altimeter
Antarctic ice sheet
Snowpack properties
Snow compaction
Radar modelling
spellingShingle Altimeter
Antarctic ice sheet
Snowpack properties
Snow compaction
Radar modelling
topic_facet Altimeter
Antarctic ice sheet
Snowpack properties
Snow compaction
Radar modelling
description with the snow surface. The backscatter coefficient of the surface is derived using the IEM method [Fung, A. K. (1994). Microwave scattering and emission models and their applications, Boston, MA: Artech House.]. The sub-surface signal takes into account both the layering effects and the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.2769
http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.2769
http://etienne.berthier.free.fr/ftp/Lacroix_et_al_RSE_2008.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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