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New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss

I. J. Nias, S. L. Cornford, A. J. Payne, Stephen Cornford Orcid Logo

Geophysical Research Letters, Volume: 45, Issue: 7, Pages: 3173 - 3181

Swansea University Author: Stephen Cornford Orcid Logo

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DOI (Published version): 10.1002/2017GL076493

Abstract

Published maps of of Antarctic bedrock elevation place Pine Island Glacier's grounding line on a submarine ridge, but observations of ice velocity indicate that the ridge is absent. Constructing a map of bedrock elevation that is compatible with the ice velocity leads to an ice sheet model that...

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Published in: Geophysical Research Letters
ISSN: 00948276
Published: 2018
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa39422
first_indexed 2018-04-16T13:41:48Z
last_indexed 2020-06-18T18:54:09Z
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spelling 2020-06-18T13:40:27.6270162 v2 39422 2018-04-16 New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss 17ae00ff2346b8c23d7e2b34341610a4 0000-0003-1844-274X Stephen Cornford Stephen Cornford true false 2018-04-16 BGPS Published maps of of Antarctic bedrock elevation place Pine Island Glacier's grounding line on a submarine ridge, but observations of ice velocity indicate that the ridge is absent. Constructing a map of bedrock elevation that is compatible with the ice velocity leads to an ice sheet model that quite different dynamic behaviour over the coming decades, and present day behaviour that is in better agreement with observations. Journal Article Geophysical Research Letters 45 7 3173 3181 00948276 16 4 2018 2018-04-16 10.1002/2017GL076493 COLLEGE NANME Biosciences Geography and Physics School COLLEGE CODE BGPS Swansea University RCUK 2020-06-18T13:40:27.6270162 2018-04-16T10:32:21.2562126 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography I. J. Nias 1 S. L. Cornford 2 A. J. Payne 3 Stephen Cornford 0000-0003-1844-274X 4 0039422-25042018202316.pdf Nias_et_al-2018-Geophysical_Research_Letters.pdf 2018-04-25T20:23:16.9870000 Output 2268523 application/pdf Version of Record true 2018-04-25T00:00:00.0000000 This is an open access article under the terms of the Creative Commons Attribution License. true eng
title New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
spellingShingle New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
Stephen Cornford
title_short New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
title_full New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
title_fullStr New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
title_full_unstemmed New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
title_sort New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
author_id_str_mv 17ae00ff2346b8c23d7e2b34341610a4
author_id_fullname_str_mv 17ae00ff2346b8c23d7e2b34341610a4_***_Stephen Cornford
author Stephen Cornford
author2 I. J. Nias
S. L. Cornford
A. J. Payne
Stephen Cornford
format Journal article
container_title Geophysical Research Letters
container_volume 45
container_issue 7
container_start_page 3173
publishDate 2018
institution Swansea University
issn 00948276
doi_str_mv 10.1002/2017GL076493
college_str Faculty of Science and Engineering
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hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
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description Published maps of of Antarctic bedrock elevation place Pine Island Glacier's grounding line on a submarine ridge, but observations of ice velocity indicate that the ridge is absent. Constructing a map of bedrock elevation that is compatible with the ice velocity leads to an ice sheet model that quite different dynamic behaviour over the coming decades, and present day behaviour that is in better agreement with observations.
published_date 2018-04-16T13:29:42Z
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