Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ...
Efforts to parameterize ice shelf basal melting within climate models are limited by an incomplete understanding of the influence of ice base slope on the turbulent ice shelf-ocean boundary current (ISOBC). Here we examine the relationship between ice base slope, boundary current dynamics, and melt...
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Online Access: | https://dx.doi.org/10.17863/cam.107991 https://www.repository.cam.ac.uk/handle/1810/367385 |
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ftdatacite:10.17863/cam.107991 2024-09-15T17:47:22+00:00 Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... Anselin, Josephine Taylor, John Holland, Paul Jenkins, Adrian Taylor, John 2024 https://dx.doi.org/10.17863/cam.107991 https://www.repository.cam.ac.uk/handle/1810/367385 en eng American Meteorological Society open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 3708 Oceanography 3709 Physical Geography and Environmental Geoscience 37 Earth Sciences 40 Engineering 4012 Fluid Mechanics and Thermal Engineering 13 Climate Action 14 Life Below Water JournalArticle Article ScholarlyArticle article-journal 2024 ftdatacite https://doi.org/10.17863/cam.107991 2024-09-02T09:07:22Z Efforts to parameterize ice shelf basal melting within climate models are limited by an incomplete understanding of the influence of ice base slope on the turbulent ice shelf-ocean boundary current (ISOBC). Here we examine the relationship between ice base slope, boundary current dynamics, and melt rate using 3-D, turbulence-permitting large-eddy simulations (LES) of an idealized ice shelf-ocean boundary current forced solely by melt-induced buoyancy. The range of simulated slopes (3-10%) is appropriate to the grounding zone of small Antarctic ice shelves and to the flanks of relatively wide ice base channels, and the initial conditions are representative of warm-cavity ocean conditions. In line with previous studies, the simulations feature the development of an Ekman boundary layer adjacent to the ice, overlaying a broad pycnocline. The time-averaged flow within the pycnocline is in thermal wind balance, with a mean shear that is only weakly dependent on the ice base slope angle alpha, resulting in a mean ... Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ice Shelves DataCite |
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Open Polar |
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DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
3708 Oceanography 3709 Physical Geography and Environmental Geoscience 37 Earth Sciences 40 Engineering 4012 Fluid Mechanics and Thermal Engineering 13 Climate Action 14 Life Below Water |
spellingShingle |
3708 Oceanography 3709 Physical Geography and Environmental Geoscience 37 Earth Sciences 40 Engineering 4012 Fluid Mechanics and Thermal Engineering 13 Climate Action 14 Life Below Water Anselin, Josephine Taylor, John Holland, Paul Jenkins, Adrian Taylor, John Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
topic_facet |
3708 Oceanography 3709 Physical Geography and Environmental Geoscience 37 Earth Sciences 40 Engineering 4012 Fluid Mechanics and Thermal Engineering 13 Climate Action 14 Life Below Water |
description |
Efforts to parameterize ice shelf basal melting within climate models are limited by an incomplete understanding of the influence of ice base slope on the turbulent ice shelf-ocean boundary current (ISOBC). Here we examine the relationship between ice base slope, boundary current dynamics, and melt rate using 3-D, turbulence-permitting large-eddy simulations (LES) of an idealized ice shelf-ocean boundary current forced solely by melt-induced buoyancy. The range of simulated slopes (3-10%) is appropriate to the grounding zone of small Antarctic ice shelves and to the flanks of relatively wide ice base channels, and the initial conditions are representative of warm-cavity ocean conditions. In line with previous studies, the simulations feature the development of an Ekman boundary layer adjacent to the ice, overlaying a broad pycnocline. The time-averaged flow within the pycnocline is in thermal wind balance, with a mean shear that is only weakly dependent on the ice base slope angle alpha, resulting in a mean ... |
format |
Article in Journal/Newspaper |
author |
Anselin, Josephine Taylor, John Holland, Paul Jenkins, Adrian Taylor, John |
author_facet |
Anselin, Josephine Taylor, John Holland, Paul Jenkins, Adrian Taylor, John |
author_sort |
Anselin, Josephine |
title |
Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
title_short |
Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
title_full |
Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
title_fullStr |
Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
title_full_unstemmed |
Ice Base Slope Effects on the Turbulent Ice Shelf–Ocean Boundary Current ... |
title_sort |
ice base slope effects on the turbulent ice shelf–ocean boundary current ... |
publisher |
American Meteorological Society |
publishDate |
2024 |
url |
https://dx.doi.org/10.17863/cam.107991 https://www.repository.cam.ac.uk/handle/1810/367385 |
genre |
Antarc* Antarctic Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Ice Shelf Ice Shelves |
op_rights |
open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.107991 |
_version_ |
1810496571171667968 |