Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams

Flow of glacial ice in the West Antarctic Ice Sheet localizes in narrow bands of fast-flowing ice streams bordered by ridges of nearly stagnant ice, but our understanding of the physical processes that generate this morphology is incomplete. Here we study the thermal and mechanical properties of ice...

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Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Suckale, Jenny, Platt, John Daniel, Perol, Thibaut, Rice, James Robert
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2014
Subjects:
Online Access:http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315
https://doi.org/10.1002/2013jf003008
id ftharvardudash:oai:dash.harvard.edu:1/12992315
record_format openpolar
spelling ftharvardudash:oai:dash.harvard.edu:1/12992315 2023-05-15T13:36:21+02:00 Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams Suckale, Jenny Platt, John Daniel Perol, Thibaut Rice, James Robert 2014 application/pdf http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315 https://doi.org/10.1002/2013jf003008 en_US eng Wiley-Blackwell doi:10.1002/2013jf003008 http://darkwing.uoregon.edu/~rempel/_readings/week6_suckale.pdf http://www.researchgate.net/profile/James_Rice9/publication/260756322_Deformation-induced_melting_in_the_margins_of_the_West-Antarctic_ice_streams/links/542852ec0cf26120b7b566e2 http://esag.harvard.edu/rice/249_SuckalePlattPerolRice_IceStreamThermomech_JGR14.pdf Journal of Geophysical Research: Earth Surface Suckale, Jenny, John D. Platt, Thibaut Perol, and James R. Rice. 2014. Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams. Journal of Geophysical Research: Earth Surface 119, no. 5: 1004–1025. 2169-9003 http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315 ice streams shear margin West Antarctica Siple Coast Dragon margin deformation-induced melting Journal Article 2014 ftharvardudash https://doi.org/10.1002/2013jf003008 2022-04-04T20:51:43Z Flow of glacial ice in the West Antarctic Ice Sheet localizes in narrow bands of fast-flowing ice streams bordered by ridges of nearly stagnant ice, but our understanding of the physical processes that generate this morphology is incomplete. Here we study the thermal and mechanical properties of ice-stream margins, where flow transitions from rapid to stagnant over a few kilometers. Our goal is to explore under which conditions the intense shear deformation in the margin may lead to deformation-induced melting. We propose a 2-D model that represents a cross section through the ice stream margin perpendicular to the downstream flow direction. We limit temperature to the melting point to estimate melt rates based on latent heat. Using rheology parameters as constrained by laboratory data and observations, we conclude that a zone of temperate ice is likely to form in active shear margins. Earth and Planetary Sciences Engineering and Applied Sciences Accepted Manuscript Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet West Antarctica Harvard University: DASH - Digital Access to Scholarship at Harvard Antarctic Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Siple Coast ENVELOPE(-155.000,-155.000,-82.000,-82.000) West Antarctic Ice Sheet West Antarctica Journal of Geophysical Research: Earth Surface 119 5 1004 1025
institution Open Polar
collection Harvard University: DASH - Digital Access to Scholarship at Harvard
op_collection_id ftharvardudash
language English
topic ice streams
shear margin
West Antarctica
Siple Coast
Dragon margin
deformation-induced melting
spellingShingle ice streams
shear margin
West Antarctica
Siple Coast
Dragon margin
deformation-induced melting
Suckale, Jenny
Platt, John Daniel
Perol, Thibaut
Rice, James Robert
Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
topic_facet ice streams
shear margin
West Antarctica
Siple Coast
Dragon margin
deformation-induced melting
description Flow of glacial ice in the West Antarctic Ice Sheet localizes in narrow bands of fast-flowing ice streams bordered by ridges of nearly stagnant ice, but our understanding of the physical processes that generate this morphology is incomplete. Here we study the thermal and mechanical properties of ice-stream margins, where flow transitions from rapid to stagnant over a few kilometers. Our goal is to explore under which conditions the intense shear deformation in the margin may lead to deformation-induced melting. We propose a 2-D model that represents a cross section through the ice stream margin perpendicular to the downstream flow direction. We limit temperature to the melting point to estimate melt rates based on latent heat. Using rheology parameters as constrained by laboratory data and observations, we conclude that a zone of temperate ice is likely to form in active shear margins. Earth and Planetary Sciences Engineering and Applied Sciences Accepted Manuscript
format Article in Journal/Newspaper
author Suckale, Jenny
Platt, John Daniel
Perol, Thibaut
Rice, James Robert
author_facet Suckale, Jenny
Platt, John Daniel
Perol, Thibaut
Rice, James Robert
author_sort Suckale, Jenny
title Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
title_short Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
title_full Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
title_fullStr Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
title_full_unstemmed Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams
title_sort deformation-induced melting in the margins of the west antarctic ice streams
publisher Wiley-Blackwell
publishDate 2014
url http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315
https://doi.org/10.1002/2013jf003008
long_lat ENVELOPE(-83.917,-83.917,-75.917,-75.917)
ENVELOPE(-155.000,-155.000,-82.000,-82.000)
geographic Antarctic
Siple
Siple Coast
West Antarctic Ice Sheet
West Antarctica
geographic_facet Antarctic
Siple
Siple Coast
West Antarctic Ice Sheet
West Antarctica
genre Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
op_relation doi:10.1002/2013jf003008
http://darkwing.uoregon.edu/~rempel/_readings/week6_suckale.pdf
http://www.researchgate.net/profile/James_Rice9/publication/260756322_Deformation-induced_melting_in_the_margins_of_the_West-Antarctic_ice_streams/links/542852ec0cf26120b7b566e2
http://esag.harvard.edu/rice/249_SuckalePlattPerolRice_IceStreamThermomech_JGR14.pdf
Journal of Geophysical Research: Earth Surface
Suckale, Jenny, John D. Platt, Thibaut Perol, and James R. Rice. 2014. Deformation-Induced Melting in the Margins of the West Antarctic Ice Streams. Journal of Geophysical Research: Earth Surface 119, no. 5: 1004–1025.
2169-9003
http://nrs.harvard.edu/urn-3:HUL.InstRepos:12992315
op_doi https://doi.org/10.1002/2013jf003008
container_title Journal of Geophysical Research: Earth Surface
container_volume 119
container_issue 5
container_start_page 1004
op_container_end_page 1025
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