Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf
Satellite-based estimates of ice shelf melt rates reach similar to 200 m yr-1 close to the grounding line of Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able to reproduce such high melt rates, even with high-resolution models. Here, we use a regional model o...
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Online Access: | http://hdl.handle.net/2115/84616 https://doi.org/10.1029/2021GL093923 |
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fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/84616 2023-05-15T13:51:33+02:00 Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf Nakayama, Yoshihiro Cai, Cilan Seroussi, Helene http://hdl.handle.net/2115/84616 https://doi.org/10.1029/2021GL093923 eng eng American Geophysical Union http://hdl.handle.net/2115/84616 Geophysical research letters, 48(18): e2021GL093923 http://dx.doi.org/10.1029/2021GL093923 Copyright 2021 American Geophysical Union. Antarctica Pine Island ice shelf subglacial freshwater discharge ice shelf melting glacial meltwater spreading 450 article fthokunivhus https://doi.org/10.1029/2021GL093923 2022-11-18T01:06:41Z Satellite-based estimates of ice shelf melt rates reach similar to 200 m yr-1 close to the grounding line of Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able to reproduce such high melt rates, even with high-resolution models. Here, we use a regional model of Pine Island ice shelf cavity and study the impact of subglacial freshwater discharge on simulated ice shelf melt rates and ocean circulation in the cavity. We show that subglacial freshwater discharge substantially enhances ice shelf melting close to the grounding line, successfully simulating high ice shelf melt rates suggested by observations. The buoyant mixture of glacial meltwater plume rises to similar to 27.4 isopycnal surfaces, following topographically constrained current, and spreads into mid-depths at the ice shelf front. The role of freshwater discharge is likely to remain unchanged over the coming decades given the projected evolution of runoff and rainfall over Pine Island basin. Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Pine Island Pine Island Glacier West Antarctica Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) West Antarctica Geophysical Research Letters 48 18 |
institution |
Open Polar |
collection |
Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) |
op_collection_id |
fthokunivhus |
language |
English |
topic |
Antarctica Pine Island ice shelf subglacial freshwater discharge ice shelf melting glacial meltwater spreading 450 |
spellingShingle |
Antarctica Pine Island ice shelf subglacial freshwater discharge ice shelf melting glacial meltwater spreading 450 Nakayama, Yoshihiro Cai, Cilan Seroussi, Helene Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
topic_facet |
Antarctica Pine Island ice shelf subglacial freshwater discharge ice shelf melting glacial meltwater spreading 450 |
description |
Satellite-based estimates of ice shelf melt rates reach similar to 200 m yr-1 close to the grounding line of Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able to reproduce such high melt rates, even with high-resolution models. Here, we use a regional model of Pine Island ice shelf cavity and study the impact of subglacial freshwater discharge on simulated ice shelf melt rates and ocean circulation in the cavity. We show that subglacial freshwater discharge substantially enhances ice shelf melting close to the grounding line, successfully simulating high ice shelf melt rates suggested by observations. The buoyant mixture of glacial meltwater plume rises to similar to 27.4 isopycnal surfaces, following topographically constrained current, and spreads into mid-depths at the ice shelf front. The role of freshwater discharge is likely to remain unchanged over the coming decades given the projected evolution of runoff and rainfall over Pine Island basin. |
format |
Article in Journal/Newspaper |
author |
Nakayama, Yoshihiro Cai, Cilan Seroussi, Helene |
author_facet |
Nakayama, Yoshihiro Cai, Cilan Seroussi, Helene |
author_sort |
Nakayama, Yoshihiro |
title |
Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
title_short |
Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
title_full |
Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
title_fullStr |
Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
title_full_unstemmed |
Impact of Subglacial Freshwater Discharge on Pine Island Ice Shelf |
title_sort |
impact of subglacial freshwater discharge on pine island ice shelf |
publisher |
American Geophysical Union |
url |
http://hdl.handle.net/2115/84616 https://doi.org/10.1029/2021GL093923 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) |
geographic |
Pine Island Glacier West Antarctica |
geographic_facet |
Pine Island Glacier West Antarctica |
genre |
Antarc* Antarctica Ice Shelf Pine Island Pine Island Glacier West Antarctica |
genre_facet |
Antarc* Antarctica Ice Shelf Pine Island Pine Island Glacier West Antarctica |
op_relation |
http://hdl.handle.net/2115/84616 Geophysical research letters, 48(18): e2021GL093923 http://dx.doi.org/10.1029/2021GL093923 |
op_rights |
Copyright 2021 American Geophysical Union. |
op_doi |
https://doi.org/10.1029/2021GL093923 |
container_title |
Geophysical Research Letters |
container_volume |
48 |
container_issue |
18 |
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1766255460698030080 |