Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...

<!--!introduction!--> Currently, in NEMO and in most ocean models, melting parameterisation below ice shelves is controlled by shear stress, which depends on the mean flow in the boundary layer and the so-called coefficient of drag. This parameter, constant in space and time, is usually tuned...

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Main Authors: Vallot, Dorothée, Jourdain, Nicolas, Mathiot, Pierre
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-2515
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019373
id ftdatacite:10.57757/iugg23-2515
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spelling ftdatacite:10.57757/iugg23-2515 2023-07-23T04:13:20+02:00 Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ... Vallot, Dorothée Jourdain, Nicolas Mathiot, Pierre 2023 https://dx.doi.org/10.57757/iugg23-2515 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019373 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2515 2023-07-03T20:54:21Z <!--!introduction!--> Currently, in NEMO and in most ocean models, melting parameterisation below ice shelves is controlled by shear stress, which depends on the mean flow in the boundary layer and the so-called coefficient of drag. This parameter, constant in space and time, is usually tuned to approach observed melt at a given ice shelf. This is equivalent to parameterise ice shelf bottoms as smooth surfaces, whereas, in reality, they can be very rough at different scales. As ice shelves are predicted to experience further damage in the future, applying a spatially varying drag might decrease uncertainties related to melt predictions below ice shelves. Here we present a study with a spatially variable coefficient of drag, which depends on the topography and on the first wet cell height. We use the ice shelf parameterisation of NEMO4.2 on a configuration of Amundsen Sea at 12 th of a degree. ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Amundsen Sea Ice Shelf Ice Shelves DataCite Metadata Store (German National Library of Science and Technology) Amundsen Sea
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> Currently, in NEMO and in most ocean models, melting parameterisation below ice shelves is controlled by shear stress, which depends on the mean flow in the boundary layer and the so-called coefficient of drag. This parameter, constant in space and time, is usually tuned to approach observed melt at a given ice shelf. This is equivalent to parameterise ice shelf bottoms as smooth surfaces, whereas, in reality, they can be very rough at different scales. As ice shelves are predicted to experience further damage in the future, applying a spatially varying drag might decrease uncertainties related to melt predictions below ice shelves. Here we present a study with a spatially variable coefficient of drag, which depends on the topography and on the first wet cell height. We use the ice shelf parameterisation of NEMO4.2 on a configuration of Amundsen Sea at 12 th of a degree. ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Vallot, Dorothée
Jourdain, Nicolas
Mathiot, Pierre
spellingShingle Vallot, Dorothée
Jourdain, Nicolas
Mathiot, Pierre
Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
author_facet Vallot, Dorothée
Jourdain, Nicolas
Mathiot, Pierre
author_sort Vallot, Dorothée
title Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
title_short Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
title_full Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
title_fullStr Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
title_full_unstemmed Spatially variable drag in the shear-controlled melt parameterisation below ice shelves in NEMO ...
title_sort spatially variable drag in the shear-controlled melt parameterisation below ice shelves in nemo ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-2515
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019373
geographic Amundsen Sea
geographic_facet Amundsen Sea
genre Amundsen Sea
Ice Shelf
Ice Shelves
genre_facet Amundsen Sea
Ice Shelf
Ice Shelves
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-2515
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