Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait
Petermann Gletscher drains ~4% of the Greenland ice sheet (GrIS) area, with ~80% of its mass loss occurring by basal melting of its ice shelf. We use a high-resolution coupled ocean and sea-ice model with a thermodynamic glacial ice shelf to diagnose ocean-controlled seasonality in basal melting of...
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Cambridge University Press
2017
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Online Access: | https://doi.org/10.1017/jog.2016.140 https://doaj.org/article/3f250c0757094bcfb6bd6c2edfd065f4 |
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ftdoajarticles:oai:doaj.org/article:3f250c0757094bcfb6bd6c2edfd065f4 2023-05-15T16:21:31+02:00 Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait E. L. SHROYER L. PADMAN R. M. SAMELSON A. MÜNCHOW L. A. STEARNS 2017-04-01T00:00:00Z https://doi.org/10.1017/jog.2016.140 https://doaj.org/article/3f250c0757094bcfb6bd6c2edfd065f4 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143016001404/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.140 0022-1430 1727-5652 https://doaj.org/article/3f250c0757094bcfb6bd6c2edfd065f4 Journal of Glaciology, Vol 63, Pp 324-330 (2017) basal melt ice shelf landfast sea ice Nares Strait ocean/glacier interactions ocean/ice interactions Petermann Gletscher sea-ice arching Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2016.140 2023-03-12T01:30:59Z Petermann Gletscher drains ~4% of the Greenland ice sheet (GrIS) area, with ~80% of its mass loss occurring by basal melting of its ice shelf. We use a high-resolution coupled ocean and sea-ice model with a thermodynamic glacial ice shelf to diagnose ocean-controlled seasonality in basal melting of the Petermann ice shelf. Basal melt rates increase by ~20% in summer due to a seasonal shift in ocean circulation within Nares Strait that is associated with the transition from landfast sea ice to mobile sea ice. Under landfast ice, cold near-surface waters are maintained on the eastern side of the strait and within Petermann Fjord, reducing basal melt and insulating the ice shelf. Under mobile sea ice, warm waters are upwelled on the eastern side of the strait and, mediated by local instabilities and eddies, enter Petermann Fjord, enhancing basal melt down to depths of 200 m. The transition between these states occurs rapidly, and seasonal changes within Nares Strait are conveyed into the fjord within the same season. These results suggest that long-term changes in the length of the landfast sea-ice season will substantially alter the structure of Petermann ice shelf and its contribution to GrIS mass loss. Article in Journal/Newspaper glacier Greenland Ice Sheet Ice Shelf Journal of Glaciology Nares strait Petermann Fjord Petermann gletscher Sea ice Directory of Open Access Journals: DOAJ Articles Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Petermann Fjord ENVELOPE(-61.500,-61.500,81.167,81.167) Petermann Gletscher ENVELOPE(-59.500,-59.500,80.500,80.500) Journal of Glaciology 63 238 324 330 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
basal melt ice shelf landfast sea ice Nares Strait ocean/glacier interactions ocean/ice interactions Petermann Gletscher sea-ice arching Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
basal melt ice shelf landfast sea ice Nares Strait ocean/glacier interactions ocean/ice interactions Petermann Gletscher sea-ice arching Environmental sciences GE1-350 Meteorology. Climatology QC851-999 E. L. SHROYER L. PADMAN R. M. SAMELSON A. MÜNCHOW L. A. STEARNS Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
topic_facet |
basal melt ice shelf landfast sea ice Nares Strait ocean/glacier interactions ocean/ice interactions Petermann Gletscher sea-ice arching Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Petermann Gletscher drains ~4% of the Greenland ice sheet (GrIS) area, with ~80% of its mass loss occurring by basal melting of its ice shelf. We use a high-resolution coupled ocean and sea-ice model with a thermodynamic glacial ice shelf to diagnose ocean-controlled seasonality in basal melting of the Petermann ice shelf. Basal melt rates increase by ~20% in summer due to a seasonal shift in ocean circulation within Nares Strait that is associated with the transition from landfast sea ice to mobile sea ice. Under landfast ice, cold near-surface waters are maintained on the eastern side of the strait and within Petermann Fjord, reducing basal melt and insulating the ice shelf. Under mobile sea ice, warm waters are upwelled on the eastern side of the strait and, mediated by local instabilities and eddies, enter Petermann Fjord, enhancing basal melt down to depths of 200 m. The transition between these states occurs rapidly, and seasonal changes within Nares Strait are conveyed into the fjord within the same season. These results suggest that long-term changes in the length of the landfast sea-ice season will substantially alter the structure of Petermann ice shelf and its contribution to GrIS mass loss. |
format |
Article in Journal/Newspaper |
author |
E. L. SHROYER L. PADMAN R. M. SAMELSON A. MÜNCHOW L. A. STEARNS |
author_facet |
E. L. SHROYER L. PADMAN R. M. SAMELSON A. MÜNCHOW L. A. STEARNS |
author_sort |
E. L. SHROYER |
title |
Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
title_short |
Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
title_full |
Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
title_fullStr |
Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
title_full_unstemmed |
Seasonal control of Petermann Gletscher ice-shelf melt by the ocean's response to sea-ice cover in Nares Strait |
title_sort |
seasonal control of petermann gletscher ice-shelf melt by the ocean's response to sea-ice cover in nares strait |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/jog.2016.140 https://doaj.org/article/3f250c0757094bcfb6bd6c2edfd065f4 |
long_lat |
ENVELOPE(158.167,158.167,-81.450,-81.450) ENVELOPE(-61.500,-61.500,81.167,81.167) ENVELOPE(-59.500,-59.500,80.500,80.500) |
geographic |
Greenland Nares Petermann Fjord Petermann Gletscher |
geographic_facet |
Greenland Nares Petermann Fjord Petermann Gletscher |
genre |
glacier Greenland Ice Sheet Ice Shelf Journal of Glaciology Nares strait Petermann Fjord Petermann gletscher Sea ice |
genre_facet |
glacier Greenland Ice Sheet Ice Shelf Journal of Glaciology Nares strait Petermann Fjord Petermann gletscher Sea ice |
op_source |
Journal of Glaciology, Vol 63, Pp 324-330 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143016001404/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.140 0022-1430 1727-5652 https://doaj.org/article/3f250c0757094bcfb6bd6c2edfd065f4 |
op_doi |
https://doi.org/10.1017/jog.2016.140 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
238 |
container_start_page |
324 |
op_container_end_page |
330 |
_version_ |
1766009528985321472 |