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:10.1.1.396.6680 2023-05-15T17:57:23+02:00 TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) Reynald Delaloye Christophe Lambiel Ralph Lugon Hugo Raetzo Tazio Strozzi The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.396.6680 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.396.6680 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://earth.esa.int/workshops/envisatsymposium/proceedings/posters/3P7/459491de.pdf text ftciteseerx 2016-01-08T02:30:57Z 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 |
language |
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. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Reynald Delaloye Christophe Lambiel Ralph Lugon Hugo Raetzo Tazio Strozzi |
spellingShingle |
Reynald Delaloye Christophe Lambiel Ralph Lugon Hugo Raetzo Tazio Strozzi TYPICAL ERS INSAR SIGNATURE OF SLOPE MOVEMENTS IN A PERIGLACIAL MOUNTAIN ENVIRONMENT (SWISS ALPS) |
author_facet |
Reynald Delaloye Christophe Lambiel Ralph Lugon Hugo Raetzo Tazio Strozzi |
author_sort |
Reynald Delaloye |
title |
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=10.1.1.396.6680 |
genre |
permafrost |
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permafrost |
op_source |
https://earth.esa.int/workshops/envisatsymposium/proceedings/posters/3P7/459491de.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.396.6680 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766165806000898048 |