Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...

Ice deformation and basal motion characterize the dynamical behavior of the Greenland ice sheet (GrIS). We evaluate the contribution of basal motion from ice deformation measurements in boreholes drilled to the bed at two sites in the western marginal zone of the GrIS. We find a sustained high amoun...

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Main Authors: Ryser, Claudia, Lüthi, Martin P., Andrews, Lauren C., Hoffman, Matthew J., Catania, Ginny A., Hawley, Robert L., Neumann, Thomas A., Kristensen, Steen S.
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2014
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000091436
http://hdl.handle.net/20.500.11850/91436
id ftdatacite:10.3929/ethz-b-000091436
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000091436 2024-04-28T08:10:23+00:00 Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ... Ryser, Claudia Lüthi, Martin P. Andrews, Lauren C. Hoffman, Matthew J. Catania, Ginny A. Hawley, Robert L. Neumann, Thomas A. Kristensen, Steen S. 2014 application/pdf https://dx.doi.org/10.3929/ethz-b-000091436 http://hdl.handle.net/20.500.11850/91436 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic glaciology Ice dynamics Ice rheology article-journal Text ScholarlyArticle Journal Article 2014 ftdatacite https://doi.org/10.3929/ethz-b-000091436 2024-04-02T12:34:54Z Ice deformation and basal motion characterize the dynamical behavior of the Greenland ice sheet (GrIS). We evaluate the contribution of basal motion from ice deformation measurements in boreholes drilled to the bed at two sites in the western marginal zone of the GrIS. We find a sustained high amount of basal motion contribution to surface velocity of 44–73% in winter, and up to 90% in summer. Measured ice deformation rates show an unexpected variation with depth that can be explained with the help of an ice-flow model as a consequence of stress transfer from slippery to sticky areas. This effect necessitates the use of high-order ice-flow models, not only in regions of fast-flowing ice streams but in all temperate-based areas of the GrIS. The agreement between modeled and measured deformation rates confirms that the recommended values of the temperature-dependent flow rate factor A are a good choice for ice-sheet models. ... : Journal of Glaciology, 60 (222) ... Article in Journal/Newspaper Arctic Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Arctic glaciology
Ice dynamics
Ice rheology
spellingShingle Arctic glaciology
Ice dynamics
Ice rheology
Ryser, Claudia
Lüthi, Martin P.
Andrews, Lauren C.
Hoffman, Matthew J.
Catania, Ginny A.
Hawley, Robert L.
Neumann, Thomas A.
Kristensen, Steen S.
Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
topic_facet Arctic glaciology
Ice dynamics
Ice rheology
description Ice deformation and basal motion characterize the dynamical behavior of the Greenland ice sheet (GrIS). We evaluate the contribution of basal motion from ice deformation measurements in boreholes drilled to the bed at two sites in the western marginal zone of the GrIS. We find a sustained high amount of basal motion contribution to surface velocity of 44–73% in winter, and up to 90% in summer. Measured ice deformation rates show an unexpected variation with depth that can be explained with the help of an ice-flow model as a consequence of stress transfer from slippery to sticky areas. This effect necessitates the use of high-order ice-flow models, not only in regions of fast-flowing ice streams but in all temperate-based areas of the GrIS. The agreement between modeled and measured deformation rates confirms that the recommended values of the temperature-dependent flow rate factor A are a good choice for ice-sheet models. ... : Journal of Glaciology, 60 (222) ...
format Article in Journal/Newspaper
author Ryser, Claudia
Lüthi, Martin P.
Andrews, Lauren C.
Hoffman, Matthew J.
Catania, Ginny A.
Hawley, Robert L.
Neumann, Thomas A.
Kristensen, Steen S.
author_facet Ryser, Claudia
Lüthi, Martin P.
Andrews, Lauren C.
Hoffman, Matthew J.
Catania, Ginny A.
Hawley, Robert L.
Neumann, Thomas A.
Kristensen, Steen S.
author_sort Ryser, Claudia
title Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
title_short Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
title_full Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
title_fullStr Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
title_full_unstemmed Sustained high basal motion of the Greenland ice sheet revealed by borehole deformation ...
title_sort sustained high basal motion of the greenland ice sheet revealed by borehole deformation ...
publisher ETH Zurich
publishDate 2014
url https://dx.doi.org/10.3929/ethz-b-000091436
http://hdl.handle.net/20.500.11850/91436
genre Arctic
Greenland
Ice Sheet
genre_facet Arctic
Greenland
Ice Sheet
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.3929/ethz-b-000091436
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