Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow

GPS measurements reveal strong modulation of horizontal ice shelf and ice stream flow at a variety of tidal frequencies, most notably a fortnightly ( M sf ) frequency not present in the vertical tides themselves. Current theories largely fail to explain the strength and prevalence of this signal ove...

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Published in:The Cryosphere
Main Authors: Rosier, Sebastian H. R., Gudmundsson, G. Hilmar
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-12-1699-2018
https://tc.copernicus.org/articles/12/1699/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc61477 2023-05-15T16:41:47+02:00 Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow Rosier, Sebastian H. R. Gudmundsson, G. Hilmar 2019-01-10 application/pdf https://doi.org/10.5194/tc-12-1699-2018 https://tc.copernicus.org/articles/12/1699/2018/ eng eng doi:10.5194/tc-12-1699-2018 https://tc.copernicus.org/articles/12/1699/2018/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-12-1699-2018 2020-07-20T16:23:18Z GPS measurements reveal strong modulation of horizontal ice shelf and ice stream flow at a variety of tidal frequencies, most notably a fortnightly ( M sf ) frequency not present in the vertical tides themselves. Current theories largely fail to explain the strength and prevalence of this signal over floating ice shelves. We show how well-known non-linear aspects of ice rheology can give rise to widespread, long-periodic tidal modulation in ice shelf flow, generated within ice shelves themselves through tidal flexure acting at diurnal and semidiurnal frequencies. Using full-Stokes viscoelastic modelling, we show that inclusion of tidal bending within the model accounts for much of the observed tidal modulation of ice shelf flow. Furthermore, our model shows that, in the absence of vertical tidal forcing, the mean flow of the ice shelf is reduced by almost 30 % for the geometry that we consider. Text Ice Shelf Ice Shelves Copernicus Publications: E-Journals The Cryosphere 12 5 1699 1713
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description GPS measurements reveal strong modulation of horizontal ice shelf and ice stream flow at a variety of tidal frequencies, most notably a fortnightly ( M sf ) frequency not present in the vertical tides themselves. Current theories largely fail to explain the strength and prevalence of this signal over floating ice shelves. We show how well-known non-linear aspects of ice rheology can give rise to widespread, long-periodic tidal modulation in ice shelf flow, generated within ice shelves themselves through tidal flexure acting at diurnal and semidiurnal frequencies. Using full-Stokes viscoelastic modelling, we show that inclusion of tidal bending within the model accounts for much of the observed tidal modulation of ice shelf flow. Furthermore, our model shows that, in the absence of vertical tidal forcing, the mean flow of the ice shelf is reduced by almost 30 % for the geometry that we consider.
format Text
author Rosier, Sebastian H. R.
Gudmundsson, G. Hilmar
spellingShingle Rosier, Sebastian H. R.
Gudmundsson, G. Hilmar
Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
author_facet Rosier, Sebastian H. R.
Gudmundsson, G. Hilmar
author_sort Rosier, Sebastian H. R.
title Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
title_short Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
title_full Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
title_fullStr Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
title_full_unstemmed Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
title_sort tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
publishDate 2019
url https://doi.org/10.5194/tc-12-1699-2018
https://tc.copernicus.org/articles/12/1699/2018/
genre Ice Shelf
Ice Shelves
genre_facet Ice Shelf
Ice Shelves
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-12-1699-2018
https://tc.copernicus.org/articles/12/1699/2018/
op_doi https://doi.org/10.5194/tc-12-1699-2018
container_title The Cryosphere
container_volume 12
container_issue 5
container_start_page 1699
op_container_end_page 1713
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