The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula

The outlet glaciers to the embayment of the Larsen-B Ice Shelf started to accelerate soon after the ice shelf disintegrated in March 2002. We analyse high resolution radar images of the TerraSAR-X satellite, launched in June 2007, to map the motion of outlet glaciers in detail. The frontal velocitie...

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Published in:The Cryosphere
Main Authors: Rott, H., Müller, F., Nagler, T., Floricioiu, D.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/tc-5-125-2011
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00027743 2023-05-15T13:36:44+02:00 The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula Rott, H. Müller, F. Nagler, T. Floricioiu, D. 2011-03 electronic https://doi.org/10.5194/tc-5-125-2011 https://noa.gwlb.de/receive/cop_mods_00027743 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027698/tc-5-125-2011.pdf https://tc.copernicus.org/articles/5/125/2011/tc-5-125-2011.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-5-125-2011 https://noa.gwlb.de/receive/cop_mods_00027743 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027698/tc-5-125-2011.pdf https://tc.copernicus.org/articles/5/125/2011/tc-5-125-2011.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2011 ftnonlinearchiv https://doi.org/10.5194/tc-5-125-2011 2022-02-08T22:48:32Z The outlet glaciers to the embayment of the Larsen-B Ice Shelf started to accelerate soon after the ice shelf disintegrated in March 2002. We analyse high resolution radar images of the TerraSAR-X satellite, launched in June 2007, to map the motion of outlet glaciers in detail. The frontal velocities are used to estimate the calving fluxes for 2008/2009. As reference for pre-collapse conditions, when the glaciers were in balanced state, the ice fluxes through the same gates are computed using ice motion maps derived from interferometric data of the ERS-1/ERS-2 satellites in 1995 and 1999. Profiles of satellite laser altimetry from ICESat, crossing the terminus of several glaciers, indicate considerable glacier thinning between 2003 and 2007/2008. This is taken into account for defining the calving cross sections. The difference between the pre- and post-collapse fluxes provides an estimate on the mass imbalance. For the Larsen-B embayment the 2008 mass deficit is estimated at 4.34 ± 1.64 Gt a−1, significantly lower than previously published values. The ice flow acceleration follows a similar pattern on the various glaciers, gradually decreasing in magnitude with distance upstream from the calving front. This suggests stress perturbation at the glacier front being the main factor for acceleration. So far there are no signs of slow-down indicating that dynamic thinning and frontal retreat will go on. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf The Cryosphere Niedersächsisches Online-Archiv NOA Antarctic Antarctic Peninsula The Cryosphere 5 1 125 134
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Rott, H.
Müller, F.
Nagler, T.
Floricioiu, D.
The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
topic_facet article
Verlagsveröffentlichung
description The outlet glaciers to the embayment of the Larsen-B Ice Shelf started to accelerate soon after the ice shelf disintegrated in March 2002. We analyse high resolution radar images of the TerraSAR-X satellite, launched in June 2007, to map the motion of outlet glaciers in detail. The frontal velocities are used to estimate the calving fluxes for 2008/2009. As reference for pre-collapse conditions, when the glaciers were in balanced state, the ice fluxes through the same gates are computed using ice motion maps derived from interferometric data of the ERS-1/ERS-2 satellites in 1995 and 1999. Profiles of satellite laser altimetry from ICESat, crossing the terminus of several glaciers, indicate considerable glacier thinning between 2003 and 2007/2008. This is taken into account for defining the calving cross sections. The difference between the pre- and post-collapse fluxes provides an estimate on the mass imbalance. For the Larsen-B embayment the 2008 mass deficit is estimated at 4.34 ± 1.64 Gt a−1, significantly lower than previously published values. The ice flow acceleration follows a similar pattern on the various glaciers, gradually decreasing in magnitude with distance upstream from the calving front. This suggests stress perturbation at the glacier front being the main factor for acceleration. So far there are no signs of slow-down indicating that dynamic thinning and frontal retreat will go on.
format Article in Journal/Newspaper
author Rott, H.
Müller, F.
Nagler, T.
Floricioiu, D.
author_facet Rott, H.
Müller, F.
Nagler, T.
Floricioiu, D.
author_sort Rott, H.
title The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
title_short The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
title_full The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
title_fullStr The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
title_full_unstemmed The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
title_sort imbalance of glaciers after disintegration of larsen-b ice shelf, antarctic peninsula
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/tc-5-125-2011
https://noa.gwlb.de/receive/cop_mods_00027743
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027698/tc-5-125-2011.pdf
https://tc.copernicus.org/articles/5/125/2011/tc-5-125-2011.pdf
geographic Antarctic
Antarctic Peninsula
geographic_facet Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
The Cryosphere
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
The Cryosphere
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-5-125-2011
https://noa.gwlb.de/receive/cop_mods_00027743
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027698/tc-5-125-2011.pdf
https://tc.copernicus.org/articles/5/125/2011/tc-5-125-2011.pdf
op_rights uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-5-125-2011
container_title The Cryosphere
container_volume 5
container_issue 1
container_start_page 125
op_container_end_page 134
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