New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis

Larsen-A ice shelf in 1995 and Larsen-B in 2002. Retreat and acceleration was observed for the glaciers above the previous Larsen-A ice shelf between 1995 and 1999 by means of 24 hour repeat pass ERS-1/ERS-2 InSAR data. Because the signal over glaciers decorrelates rapidly, no InSAR analysis was pos...

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Bibliographic Details
Main Authors: Rott, Helmut, Eineder, Michael, Nagler, Thomas, Floricioiu, Dana
Format: Conference Object
Language:unknown
Published: VDE Conference Services 2008
Subjects:
Online Access:https://elib.dlr.de/53050/
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author Rott, Helmut
Eineder, Michael
Nagler, Thomas
Floricioiu, Dana
author_facet Rott, Helmut
Eineder, Michael
Nagler, Thomas
Floricioiu, Dana
author_sort Rott, Helmut
collection Unknown
description Larsen-A ice shelf in 1995 and Larsen-B in 2002. Retreat and acceleration was observed for the glaciers above the previous Larsen-A ice shelf between 1995 and 1999 by means of 24 hour repeat pass ERS-1/ERS-2 InSAR data. Because the signal over glaciers decorrelates rapidly, no InSAR analysis was possible later on with ASAR. New opportunities for ice dynamic studies were opened up by TerraSAR-X. We applied image correlation techniques with 11-day repeat pass data, acquired in strip-map mode with 3m x 3m resolution to map ice motion. Up to eight-fold acceleration of the terminal parts of glaciers was observed since the ice shelf collapse, resulting in significant increase of export of grounded ice which contributes to sea level rise. These investigations demonstrate that TerraSAR-X offers unique opportunities for studies of flow dynamics of glaciers and ice streams. The high spatial resolution and short repeat observation capabilities enable detailed observations of complex flow fields and their temporal variations.
format Conference Object
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
geographic Antarctic
Antarctic Peninsula
Asar
geographic_facet Antarctic
Antarctic Peninsula
Asar
id ftdlr:oai:elib.dlr.de:53050
institution Open Polar
language unknown
long_lat ENVELOPE(134.033,134.033,68.667,68.667)
op_collection_id ftdlr
op_relation Rott, Helmut und Eineder, Michael und Nagler, Thomas und Floricioiu, Dana (2008) New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis. In: European Conference on Synthetic Aperture Radar (EUSAR), Seiten 1-4. VDE Conference Services. EUSAR 2008, 2007-06-02 - 2007-06-05, Friedrichshafen, Germany.
publishDate 2008
publisher VDE Conference Services
record_format openpolar
spelling ftdlr:oai:elib.dlr.de:53050 2025-06-15T14:10:57+00:00 New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis Rott, Helmut Eineder, Michael Nagler, Thomas Floricioiu, Dana 2008-06-02 https://elib.dlr.de/53050/ unknown VDE Conference Services Rott, Helmut und Eineder, Michael und Nagler, Thomas und Floricioiu, Dana (2008) New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis. In: European Conference on Synthetic Aperture Radar (EUSAR), Seiten 1-4. VDE Conference Services. EUSAR 2008, 2007-06-02 - 2007-06-05, Friedrichshafen, Germany. Institut für Methodik der Fernerkundung Konferenzbeitrag NonPeerReviewed 2008 ftdlr 2025-06-04T04:58:08Z Larsen-A ice shelf in 1995 and Larsen-B in 2002. Retreat and acceleration was observed for the glaciers above the previous Larsen-A ice shelf between 1995 and 1999 by means of 24 hour repeat pass ERS-1/ERS-2 InSAR data. Because the signal over glaciers decorrelates rapidly, no InSAR analysis was possible later on with ASAR. New opportunities for ice dynamic studies were opened up by TerraSAR-X. We applied image correlation techniques with 11-day repeat pass data, acquired in strip-map mode with 3m x 3m resolution to map ice motion. Up to eight-fold acceleration of the terminal parts of glaciers was observed since the ice shelf collapse, resulting in significant increase of export of grounded ice which contributes to sea level rise. These investigations demonstrate that TerraSAR-X offers unique opportunities for studies of flow dynamics of glaciers and ice streams. The high spatial resolution and short repeat observation capabilities enable detailed observations of complex flow fields and their temporal variations. Conference Object Antarc* Antarctic Antarctic Peninsula Ice Shelf Unknown Antarctic Antarctic Peninsula Asar ENVELOPE(134.033,134.033,68.667,68.667)
spellingShingle Institut für Methodik der Fernerkundung
Rott, Helmut
Eineder, Michael
Nagler, Thomas
Floricioiu, Dana
New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title_full New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title_fullStr New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title_full_unstemmed New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title_short New results on dynamic instability of Antarctic Peninsula glaciers detected by TerraSAR-X ice motion analysis
title_sort new results on dynamic instability of antarctic peninsula glaciers detected by terrasar-x ice motion analysis
topic Institut für Methodik der Fernerkundung
topic_facet Institut für Methodik der Fernerkundung
url https://elib.dlr.de/53050/