On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms

We investigate limitations of the one-dimensional elastic beam model to detect grounding line and thickness of an ice shelf from a differential interferogram. Spatial limitations due to grounding line curvature and variable ice thickness are analyzed by comparison with two-dimensional plate flexure....

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Bibliographic Details
Main Authors: Rabus, Bernd, Lang, Oliver
Format: Article in Journal/Newspaper
Language:unknown
Published: 2002
Subjects:
Online Access:https://elib.dlr.de/390/
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spelling ftdlr:oai:elib.dlr.de:390 2024-09-15T17:40:17+00:00 On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms Rabus, Bernd Lang, Oliver 2002 https://elib.dlr.de/390/ unknown Rabus, Bernd und Lang, Oliver (2002) On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms. Journal of Glaciology, Vol. 48 (No. 162), Seiten 345-356. Deutsches Fernerkundungsdatenzentrum Zeitschriftenbeitrag PeerReviewed 2002 ftdlr 2024-07-26T03:56:15Z We investigate limitations of the one-dimensional elastic beam model to detect grounding line and thickness of an ice shelf from a differential interferogram. Spatial limitations due to grounding line curvature and variable ice thickness are analyzed by comparison with two-dimensional plate flexure. Temporal limitations from the tide-dependent shift of the grounding line are analyzed by superpositions of four tidal flexure profiles representing differential interferograms. (i) At scales greater one ice thickness seaward protrusions of the grounding line are well represented by the elastic beam model, while landward embayments of the same scale produce significant misplacements >10 per cent of the ice thickness. (ii) For reasonable spatial variations of shelf thickness the elastic beam model gives reliable estimates of grounding line position and unfractured mean ice thickness near the grounding line. (iii) For about 20 per cent of superpositions of four tidal flexure profiles the resulting grounding line misplacements exceed the physical tidal shift of the grounding line by factors >2. For differential tide levels <10 per cent of a 1 m tide dynamics, a physical shift of the grounding line of 0.3 km per meter of tide can lever misplacements of >2 km. Examples of real interferometric profiles from West Antarctic ice shelves corroborate our results. Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ice Shelves Journal of Glaciology German Aerospace Center: elib - DLR electronic library
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language unknown
topic Deutsches Fernerkundungsdatenzentrum
spellingShingle Deutsches Fernerkundungsdatenzentrum
Rabus, Bernd
Lang, Oliver
On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
topic_facet Deutsches Fernerkundungsdatenzentrum
description We investigate limitations of the one-dimensional elastic beam model to detect grounding line and thickness of an ice shelf from a differential interferogram. Spatial limitations due to grounding line curvature and variable ice thickness are analyzed by comparison with two-dimensional plate flexure. Temporal limitations from the tide-dependent shift of the grounding line are analyzed by superpositions of four tidal flexure profiles representing differential interferograms. (i) At scales greater one ice thickness seaward protrusions of the grounding line are well represented by the elastic beam model, while landward embayments of the same scale produce significant misplacements >10 per cent of the ice thickness. (ii) For reasonable spatial variations of shelf thickness the elastic beam model gives reliable estimates of grounding line position and unfractured mean ice thickness near the grounding line. (iii) For about 20 per cent of superpositions of four tidal flexure profiles the resulting grounding line misplacements exceed the physical tidal shift of the grounding line by factors >2. For differential tide levels <10 per cent of a 1 m tide dynamics, a physical shift of the grounding line of 0.3 km per meter of tide can lever misplacements of >2 km. Examples of real interferometric profiles from West Antarctic ice shelves corroborate our results.
format Article in Journal/Newspaper
author Rabus, Bernd
Lang, Oliver
author_facet Rabus, Bernd
Lang, Oliver
author_sort Rabus, Bernd
title On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
title_short On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
title_full On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
title_fullStr On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
title_full_unstemmed On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms
title_sort on the representation of ice shelf grounding zones in sar-interferograms
publishDate 2002
url https://elib.dlr.de/390/
genre Antarc*
Antarctic
Ice Shelf
Ice Shelves
Journal of Glaciology
genre_facet Antarc*
Antarctic
Ice Shelf
Ice Shelves
Journal of Glaciology
op_relation Rabus, Bernd und Lang, Oliver (2002) On the Representation of Ice Shelf Grounding Zones in SAR-Interferograms. Journal of Glaciology, Vol. 48 (No. 162), Seiten 345-356.
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