Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams

Geodetic surveys suggest that ocean tides can modulate the motion of Antarctic ice streams, even at stations many tens of kilometers inland from the grounding line. These surveys suggest that ocean tidal stresses can perturb ice stream motion at distances about an order of magnitude farther inland t...

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Main Authors: Thompson, J., Simons, M., Tsai, V. C.
Format: Article in Journal/Newspaper
Language:unknown
Published: European Geosciences Union 2014
Subjects:
Online Access:https://doi.org/10.5194/tc-8-2007-2014
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spelling ftcaltechauth:oai:authors.library.caltech.edu:2cqk9-6y547 2024-06-23T07:47:50+00:00 Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams Thompson, J. Simons, M. Tsai, V. C. 2014-11-05 https://doi.org/10.5194/tc-8-2007-2014 unknown European Geosciences Union https://doi.org/10.5194/tcd-8-2119-2014 https://doi.org/10.5194/tc-8-2007-2014 oai:authors.library.caltech.edu:2cqk9-6y547 eprintid:46343 resolverid:CaltechAUTHORS:20140618-141557404 info:eu-repo/semantics/openAccess Other Cryosphere, 8(6), 2007-2029, (2014-11-05) info:eu-repo/semantics/article 2014 ftcaltechauth https://doi.org/10.5194/tc-8-2007-201410.5194/tcd-8-2119-2014 2024-06-12T03:59:00Z Geodetic surveys suggest that ocean tides can modulate the motion of Antarctic ice streams, even at stations many tens of kilometers inland from the grounding line. These surveys suggest that ocean tidal stresses can perturb ice stream motion at distances about an order of magnitude farther inland than tidal flexure of the ice stream alone. Recent models exploring the role of tidal perturbations in basal shear stress are primarily one- or two-dimensional, with the impact of the ice stream margins either ignored or parameterized. Here, we use two- and three-dimensional finite-element modeling to investigate transmission of tidal stresses in ice streams and the impact of considering more realistic, three-dimensional ice stream geometries. Using Rutford Ice Stream as a real-world comparison, we demonstrate that the assumption that elastic tidal stresses in ice streams propagate large distances inland fails for channelized glaciers due to an intrinsic, exponential decay in the stress caused by resistance at the ice stream margins. This behavior is independent of basal conditions beneath the ice stream and cannot be fit to observations using either elastic or nonlinear viscoelastic rheologies without nearly complete decoupling of the ice stream from its lateral margins. Our results suggest that a mechanism external to the ice stream is necessary to explain the tidal modulation of stresses far upstream of the grounding line for narrow ice streams. We propose a hydrologic model based on time-dependent variability in till strength to explain transmission of tidal stresses inland of the grounding line. This conceptual model can reproduce observations from Rutford Ice Stream. © 2014 Author(s). This work is distributed under the Creative Commons Attribution 3.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union. Received: 21 February 2014 – Published in The Cryosphere Discuss.: 25 April 2014; Revised: 18 September 2014 – Accepted: 22 September 2014 – Published: 5 November ... Article in Journal/Newspaper Antarc* Antarctic Rutford Ice Stream Caltech Authors (California Institute of Technology) Antarctic Rutford ENVELOPE(-85.300,-85.300,-78.600,-78.600) Rutford Ice Stream ENVELOPE(-80.000,-80.000,-79.167,-79.167)
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description Geodetic surveys suggest that ocean tides can modulate the motion of Antarctic ice streams, even at stations many tens of kilometers inland from the grounding line. These surveys suggest that ocean tidal stresses can perturb ice stream motion at distances about an order of magnitude farther inland than tidal flexure of the ice stream alone. Recent models exploring the role of tidal perturbations in basal shear stress are primarily one- or two-dimensional, with the impact of the ice stream margins either ignored or parameterized. Here, we use two- and three-dimensional finite-element modeling to investigate transmission of tidal stresses in ice streams and the impact of considering more realistic, three-dimensional ice stream geometries. Using Rutford Ice Stream as a real-world comparison, we demonstrate that the assumption that elastic tidal stresses in ice streams propagate large distances inland fails for channelized glaciers due to an intrinsic, exponential decay in the stress caused by resistance at the ice stream margins. This behavior is independent of basal conditions beneath the ice stream and cannot be fit to observations using either elastic or nonlinear viscoelastic rheologies without nearly complete decoupling of the ice stream from its lateral margins. Our results suggest that a mechanism external to the ice stream is necessary to explain the tidal modulation of stresses far upstream of the grounding line for narrow ice streams. We propose a hydrologic model based on time-dependent variability in till strength to explain transmission of tidal stresses inland of the grounding line. This conceptual model can reproduce observations from Rutford Ice Stream. © 2014 Author(s). This work is distributed under the Creative Commons Attribution 3.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union. Received: 21 February 2014 – Published in The Cryosphere Discuss.: 25 April 2014; Revised: 18 September 2014 – Accepted: 22 September 2014 – Published: 5 November ...
format Article in Journal/Newspaper
author Thompson, J.
Simons, M.
Tsai, V. C.
spellingShingle Thompson, J.
Simons, M.
Tsai, V. C.
Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
author_facet Thompson, J.
Simons, M.
Tsai, V. C.
author_sort Thompson, J.
title Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
title_short Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
title_full Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
title_fullStr Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
title_full_unstemmed Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
title_sort modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
publisher European Geosciences Union
publishDate 2014
url https://doi.org/10.5194/tc-8-2007-2014
long_lat ENVELOPE(-85.300,-85.300,-78.600,-78.600)
ENVELOPE(-80.000,-80.000,-79.167,-79.167)
geographic Antarctic
Rutford
Rutford Ice Stream
geographic_facet Antarctic
Rutford
Rutford Ice Stream
genre Antarc*
Antarctic
Rutford Ice Stream
genre_facet Antarc*
Antarctic
Rutford Ice Stream
op_source Cryosphere, 8(6), 2007-2029, (2014-11-05)
op_relation https://doi.org/10.5194/tcd-8-2119-2014
https://doi.org/10.5194/tc-8-2007-2014
oai:authors.library.caltech.edu:2cqk9-6y547
eprintid:46343
resolverid:CaltechAUTHORS:20140618-141557404
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.5194/tc-8-2007-201410.5194/tcd-8-2119-2014
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