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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Main Authors: Anselin, Josephine, Taylor, John, Holland, Paul, Jenkins, Adrian
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2024
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.107991
https://www.repository.cam.ac.uk/handle/1810/367385
id ftdatacite:10.17863/cam.107991
record_format openpolar
spelling 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
institution Open Polar
collection 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
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