TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS)
ERS InSAR has been used for mapping and assessing slope movements in an alpine periglacial test region. A large number of areas have thus been recognized as affected by mass wasting related to permafrost or not. Glaciers and most of the active geomorphic landforms display in fact typical ERS InSAR s...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.511.5563 2023-05-15T17:57:23+02:00 TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.5563 http://my.unil.ch/serval/document/bib_736732fa6f53.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.5563 http://my.unil.ch/serval/document/bib_736732fa6f53.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://my.unil.ch/serval/document/bib_736732fa6f53.pdf text ftciteseerx 2016-01-08T09:40:11Z ERS InSAR has been used for mapping and assessing slope movements in an alpine periglacial test region. A large number of areas have thus been recognized as affected by mass wasting related to permafrost or not. Glaciers and most of the active geomorphic landforms display in fact typical ERS InSAR signals. A typology has been established. It can be seen as a useful tool to interpret ERS InSAR data in such a mountain environment. 1. Text permafrost Unknown |
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Open Polar |
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ftciteseerx |
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English |
description |
ERS InSAR has been used for mapping and assessing slope movements in an alpine periglacial test region. A large number of areas have thus been recognized as affected by mass wasting related to permafrost or not. Glaciers and most of the active geomorphic landforms display in fact typical ERS InSAR signals. A typology has been established. It can be seen as a useful tool to interpret ERS InSAR data in such a mountain environment. 1. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
spellingShingle |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
title_short |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
title_full |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
title_fullStr |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
title_full_unstemmed |
TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
title_sort |
typical ers insar signature of slope movements in a periglacial mountain environment (swiss alps) |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.5563 http://my.unil.ch/serval/document/bib_736732fa6f53.pdf |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
http://my.unil.ch/serval/document/bib_736732fa6f53.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.5563 http://my.unil.ch/serval/document/bib_736732fa6f53.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766165811271041024 |