Ice-shelf ocean boundary layer dynamics from large-eddy simulations

Small-scale turbulent flow below ice shelves is regionally isolated and difficult to measure and simulate. Yet these small-scale processes, which regulate heat and salt transfer between the ocean and ice shelves, can affect sea-level rise by altering the ability of Antarctic ice shelves to “buttress...

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Published in:The Cryosphere
Main Authors: Begeman, Carolyn Branecky, Asay-Davis, Xylar, Roekel, Luke
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-277-2022
https://tc.copernicus.org/articles/16/277/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:tc96703 2023-05-15T14:02:17+02:00 Ice-shelf ocean boundary layer dynamics from large-eddy simulations Begeman, Carolyn Branecky Asay-Davis, Xylar Roekel, Luke 2022-01-24 application/pdf https://doi.org/10.5194/tc-16-277-2022 https://tc.copernicus.org/articles/16/277/2022/ eng eng doi:10.5194/tc-16-277-2022 https://tc.copernicus.org/articles/16/277/2022/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-16-277-2022 2022-01-31T17:22:16Z Small-scale turbulent flow below ice shelves is regionally isolated and difficult to measure and simulate. Yet these small-scale processes, which regulate heat and salt transfer between the ocean and ice shelves, can affect sea-level rise by altering the ability of Antarctic ice shelves to “buttress” ice flux to the ocean. In this study, we improve our understanding of turbulence below ice shelves by means of large-eddy simulations at sub-meter resolution, capturing boundary layer mixing at scales intermediate between laboratory experiments or direct numerical simulations and regional or global ocean circulation models. Our simulations feature the development of an ice-shelf ocean boundary layer through dynamic ice melting in a regime with low thermal driving, low ice-shelf basal slope, and strong shear driven by the geostrophic flow. We present a preliminary assessment of existing ice-shelf basal melt parameterizations adopted in single component or coupled ice-sheet and ocean models on the basis of a small parameter study. While the parameterized linear relationship between ice-shelf melt rate and far-field ocean temperature appears to be robust, we point out a little-considered relationship between ice-shelf basal slope and melting worthy of further study. Text Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Copernicus Publications: E-Journals Antarctic Buttress ENVELOPE(-57.083,-57.083,-63.550,-63.550) The Cryosphere 16 1 277 295
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Small-scale turbulent flow below ice shelves is regionally isolated and difficult to measure and simulate. Yet these small-scale processes, which regulate heat and salt transfer between the ocean and ice shelves, can affect sea-level rise by altering the ability of Antarctic ice shelves to “buttress” ice flux to the ocean. In this study, we improve our understanding of turbulence below ice shelves by means of large-eddy simulations at sub-meter resolution, capturing boundary layer mixing at scales intermediate between laboratory experiments or direct numerical simulations and regional or global ocean circulation models. Our simulations feature the development of an ice-shelf ocean boundary layer through dynamic ice melting in a regime with low thermal driving, low ice-shelf basal slope, and strong shear driven by the geostrophic flow. We present a preliminary assessment of existing ice-shelf basal melt parameterizations adopted in single component or coupled ice-sheet and ocean models on the basis of a small parameter study. While the parameterized linear relationship between ice-shelf melt rate and far-field ocean temperature appears to be robust, we point out a little-considered relationship between ice-shelf basal slope and melting worthy of further study.
format Text
author Begeman, Carolyn Branecky
Asay-Davis, Xylar
Roekel, Luke
spellingShingle Begeman, Carolyn Branecky
Asay-Davis, Xylar
Roekel, Luke
Ice-shelf ocean boundary layer dynamics from large-eddy simulations
author_facet Begeman, Carolyn Branecky
Asay-Davis, Xylar
Roekel, Luke
author_sort Begeman, Carolyn Branecky
title Ice-shelf ocean boundary layer dynamics from large-eddy simulations
title_short Ice-shelf ocean boundary layer dynamics from large-eddy simulations
title_full Ice-shelf ocean boundary layer dynamics from large-eddy simulations
title_fullStr Ice-shelf ocean boundary layer dynamics from large-eddy simulations
title_full_unstemmed Ice-shelf ocean boundary layer dynamics from large-eddy simulations
title_sort ice-shelf ocean boundary layer dynamics from large-eddy simulations
publishDate 2022
url https://doi.org/10.5194/tc-16-277-2022
https://tc.copernicus.org/articles/16/277/2022/
long_lat ENVELOPE(-57.083,-57.083,-63.550,-63.550)
geographic Antarctic
Buttress
geographic_facet Antarctic
Buttress
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-16-277-2022
https://tc.copernicus.org/articles/16/277/2022/
op_doi https://doi.org/10.5194/tc-16-277-2022
container_title The Cryosphere
container_volume 16
container_issue 1
container_start_page 277
op_container_end_page 295
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