A high-resolution bedrock map for the Antarctic Peninsula

Assessing and projecting the dynamic response of glaciers on the Antarctic Peninsula to changed atmospheric and oceanic forcing requires high-resolution ice thickness data as an essential geometric constraint for ice flow models. Here, we derive a complete bedrock data set for the Antarctic Peninsul...

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Main Authors: M. Huss, D. Farinotti
Format: Article
Language:English
Published: Copernicus Publications 2014-07-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/8/1261/2014/tc-8-1261-2014.pdf
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author M. Huss
D. Farinotti
author_facet M. Huss
D. Farinotti
author_sort M. Huss
collection DOAJ
description Assessing and projecting the dynamic response of glaciers on the Antarctic Peninsula to changed atmospheric and oceanic forcing requires high-resolution ice thickness data as an essential geometric constraint for ice flow models. Here, we derive a complete bedrock data set for the Antarctic Peninsula north of 70° S on a 100 m grid. We calculate distributed ice thickness based on surface topography and simple ice dynamic modelling. Our approach is constrained with all available thickness measurements from Operation IceBridge and gridded ice flow speeds for the entire study region. The new data set resolves the rugged subglacial topography in great detail, indicates deeply incised troughs, and shows that 34% of the ice volume is grounded below sea level. The Antarctic Peninsula has the potential to raise global sea level by 69 ± 5 mm. In comparison to Bedmap2, covering all Antarctica on a 1 km grid, a significantly higher mean ice thickness (+48%) is found.
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spelling doaj.art-04100345a7d44952841c237f125092fa2022-12-21T17:45:22ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242014-07-01841261127310.5194/tc-8-1261-2014A high-resolution bedrock map for the Antarctic PeninsulaM. Huss0D. Farinotti1Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, 8093 Zurich, SwitzerlandGerman Research Centre for Geosciences (GFZ), Telegrafenberg, 14473 Potsdam, GermanyAssessing and projecting the dynamic response of glaciers on the Antarctic Peninsula to changed atmospheric and oceanic forcing requires high-resolution ice thickness data as an essential geometric constraint for ice flow models. Here, we derive a complete bedrock data set for the Antarctic Peninsula north of 70° S on a 100 m grid. We calculate distributed ice thickness based on surface topography and simple ice dynamic modelling. Our approach is constrained with all available thickness measurements from Operation IceBridge and gridded ice flow speeds for the entire study region. The new data set resolves the rugged subglacial topography in great detail, indicates deeply incised troughs, and shows that 34% of the ice volume is grounded below sea level. The Antarctic Peninsula has the potential to raise global sea level by 69 ± 5 mm. In comparison to Bedmap2, covering all Antarctica on a 1 km grid, a significantly higher mean ice thickness (+48%) is found.http://www.the-cryosphere.net/8/1261/2014/tc-8-1261-2014.pdf
spellingShingle M. Huss
D. Farinotti
A high-resolution bedrock map for the Antarctic Peninsula
The Cryosphere
title A high-resolution bedrock map for the Antarctic Peninsula
title_full A high-resolution bedrock map for the Antarctic Peninsula
title_fullStr A high-resolution bedrock map for the Antarctic Peninsula
title_full_unstemmed A high-resolution bedrock map for the Antarctic Peninsula
title_short A high-resolution bedrock map for the Antarctic Peninsula
title_sort high resolution bedrock map for the antarctic peninsula
url http://www.the-cryosphere.net/8/1261/2014/tc-8-1261-2014.pdf
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