Fracture-induced softening for large-scale ice dynamics

Floating ice shelves can exert a retentive and hence stabilizing force onto the inland ice sheet of Antarctica. However, this effect has been observed to diminish by the dynamic effects of fracture processes within the protective ice shelves, leading to accelerated ice flow and hence to a sea-level...

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Published in:The Cryosphere
Main Authors: Albrecht, Torsten, Levermann, Anders (Prof. Dr.)
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38289
https://doi.org/10.5194/tc-8-587-2014
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:38289 2024-04-21T07:50:00+00:00 Fracture-induced softening for large-scale ice dynamics Albrecht, Torsten Levermann, Anders (Prof. Dr.) 2014 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38289 https://doi.org/10.5194/tc-8-587-2014 eng eng https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38289 https://doi.org/10.5194/tc-8-587-2014 info:eu-repo/semantics/closedAccess Institut für Physik und Astronomie article doc-type:article 2014 ftubpotsdam https://doi.org/10.5194/tc-8-587-2014 2024-03-27T15:02:48Z Floating ice shelves can exert a retentive and hence stabilizing force onto the inland ice sheet of Antarctica. However, this effect has been observed to diminish by the dynamic effects of fracture processes within the protective ice shelves, leading to accelerated ice flow and hence to a sea-level contribution. In order to account for the macroscopic effect of fracture processes on large-scale viscous ice dynamics (i.e., ice-shelf scale) we apply a continuum representation of fractures and related fracture growth into the prognostic Parallel Ice Sheet Model (PISM) and compare the results to observations. To this end we introduce a higher order accuracy advection scheme for the transport of the two-dimensional fracture density across the regular computational grid. Dynamic coupling of fractures and ice flow is attained by a reduction of effective ice viscosity proportional to the inferred fracture density. This formulation implies the possibility of non-linear threshold behavior due to self-amplified fracturing in shear regions triggered by small variations in the fracture-initiation threshold. As a result of prognostic flow simulations, sharp across-flow velocity gradients appear in fracture-weakened regions. These modeled gradients compare well in magnitude and location with those in observed flow patterns. This model framework is in principle expandable to grounded ice streams and provides simple means of investigating climate-induced effects on fracturing (e. g., hydro fracturing) and hence on the ice flow. It further constitutes a physically sound basis for an enhanced fracture-based calving parameterization. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf Ice Shelves University of Potsdam: publish.UP The Cryosphere 8 2 587 605
institution Open Polar
collection University of Potsdam: publish.UP
op_collection_id ftubpotsdam
language English
topic Institut für Physik und Astronomie
spellingShingle Institut für Physik und Astronomie
Albrecht, Torsten
Levermann, Anders (Prof. Dr.)
Fracture-induced softening for large-scale ice dynamics
topic_facet Institut für Physik und Astronomie
description Floating ice shelves can exert a retentive and hence stabilizing force onto the inland ice sheet of Antarctica. However, this effect has been observed to diminish by the dynamic effects of fracture processes within the protective ice shelves, leading to accelerated ice flow and hence to a sea-level contribution. In order to account for the macroscopic effect of fracture processes on large-scale viscous ice dynamics (i.e., ice-shelf scale) we apply a continuum representation of fractures and related fracture growth into the prognostic Parallel Ice Sheet Model (PISM) and compare the results to observations. To this end we introduce a higher order accuracy advection scheme for the transport of the two-dimensional fracture density across the regular computational grid. Dynamic coupling of fractures and ice flow is attained by a reduction of effective ice viscosity proportional to the inferred fracture density. This formulation implies the possibility of non-linear threshold behavior due to self-amplified fracturing in shear regions triggered by small variations in the fracture-initiation threshold. As a result of prognostic flow simulations, sharp across-flow velocity gradients appear in fracture-weakened regions. These modeled gradients compare well in magnitude and location with those in observed flow patterns. This model framework is in principle expandable to grounded ice streams and provides simple means of investigating climate-induced effects on fracturing (e. g., hydro fracturing) and hence on the ice flow. It further constitutes a physically sound basis for an enhanced fracture-based calving parameterization.
format Article in Journal/Newspaper
author Albrecht, Torsten
Levermann, Anders (Prof. Dr.)
author_facet Albrecht, Torsten
Levermann, Anders (Prof. Dr.)
author_sort Albrecht, Torsten
title Fracture-induced softening for large-scale ice dynamics
title_short Fracture-induced softening for large-scale ice dynamics
title_full Fracture-induced softening for large-scale ice dynamics
title_fullStr Fracture-induced softening for large-scale ice dynamics
title_full_unstemmed Fracture-induced softening for large-scale ice dynamics
title_sort fracture-induced softening for large-scale ice dynamics
publishDate 2014
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38289
https://doi.org/10.5194/tc-8-587-2014
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
op_relation https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38289
https://doi.org/10.5194/tc-8-587-2014
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.5194/tc-8-587-2014
container_title The Cryosphere
container_volume 8
container_issue 2
container_start_page 587
op_container_end_page 605
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