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New Mass-Conserving Bedrock Topography for Pine Island Glacier Impacts Simulated Decadal Rates of Mass Loss
Geophysical Research Letters, Volume: 45, Issue: 7, Pages: 3173 - 3181
Swansea University Author: Stephen Cornford
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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...
Published in: | Geophysical Research Letters |
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ISSN: | 00948276 |
Published: |
2018
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Online Access: |
Check full text
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URI: | https://cronfa.swan.ac.uk/Record/cronfa39422 |
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 quite different dynamic behaviour over the coming decades, and present day behaviour that is in better agreement with observations. |
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College: |
Faculty of Science and Engineering |
Issue: |
7 |
Start Page: |
3173 |
End Page: |
3181 |