Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution
The ice shelf-ocean boundary current has an important control on heat delivery to the base of an ice shelf. Climate and regional models that include a representation of ice shelf cavities often use a coarse grid and results have a strong dependence on resolution near the ice shelf-ocean interface. T...
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American Meteorological Society
2023
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Online Access: | https://centaur.reading.ac.uk/108923/ https://centaur.reading.ac.uk/108923/1/1520-0485-JPO-D-22-0034.1.pdf |
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ftunivreading:oai:centaur.reading.ac.uk:108923 2023-09-05T13:20:20+02:00 Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution Patmore, Ryan D. Holland, Paul R. Vreugdenhil, Catherine A. Jenkins, Adrian Taylor, John R. 2023 text https://centaur.reading.ac.uk/108923/ https://centaur.reading.ac.uk/108923/1/1520-0485-JPO-D-22-0034.1.pdf en eng American Meteorological Society https://centaur.reading.ac.uk/108923/1/1520-0485-JPO-D-22-0034.1.pdf Patmore, Ryan D. ORCID logoorcid:0000-0002-5571-9229 , Holland, Paul R., Vreugdenhil, Catherine A., Jenkins, Adrian and Taylor, John R. (2023) Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution. Journal of Physical Oceanography, 53 (2). pp. 613-633. ISSN 1520-0485 doi: https://doi.org/10.1175/jpo-d-22-0034.1 <https://doi.org/10.1175/jpo-d-22-0034.1> cc_by_4 Article PeerReviewed 2023 ftunivreading https://doi.org/10.1175/jpo-d-22-0034.1 2023-08-14T18:17:41Z The ice shelf-ocean boundary current has an important control on heat delivery to the base of an ice shelf. Climate and regional models that include a representation of ice shelf cavities often use a coarse grid and results have a strong dependence on resolution near the ice shelf-ocean interface. This study models the ice shelf-ocean boundary current with a non-hydrostatic z-level configuration at turbulence-permitting resolution (1 m). The z-level model performs well when compared against state-of-the-art Large Eddy Simulations showing its capability in representing the correct physics. We showthat theoretical results from a one-dimensional model with parameterised turbulence reproduce the z-level model results to a good degree, indicating possible utility as a turbulence closure. The one-dimensional model evolves to a state of marginal instability and we use the z-level model to demonstrate how this is represented in three-dimensions. Instabilities emerge that regulate the strength of the pycnocline and coexist with persistent Ekman rolls, which are identified prior to the flow becoming intermittently unstable. When resolution of the z-level model is degraded to understand the grid-scale dependencies, the degradation is dominated by the established problem of excessive numerical diffusion. We show that at intermediate resolutions (2-4 m), the boundary layer structure can be partially recovered by tuning diffusivities. Lastly, we compare replacing prescribed melting with interactive melting that is dependent on the local ocean conditions. Interactive melting results in a feedback such that the system evolves more slowly, which is exaggerated at lower resolution. Article in Journal/Newspaper Ice Shelf CentAUR: Central Archive at the University of Reading Journal of Physical Oceanography 53 2 613 633 |
institution |
Open Polar |
collection |
CentAUR: Central Archive at the University of Reading |
op_collection_id |
ftunivreading |
language |
English |
description |
The ice shelf-ocean boundary current has an important control on heat delivery to the base of an ice shelf. Climate and regional models that include a representation of ice shelf cavities often use a coarse grid and results have a strong dependence on resolution near the ice shelf-ocean interface. This study models the ice shelf-ocean boundary current with a non-hydrostatic z-level configuration at turbulence-permitting resolution (1 m). The z-level model performs well when compared against state-of-the-art Large Eddy Simulations showing its capability in representing the correct physics. We showthat theoretical results from a one-dimensional model with parameterised turbulence reproduce the z-level model results to a good degree, indicating possible utility as a turbulence closure. The one-dimensional model evolves to a state of marginal instability and we use the z-level model to demonstrate how this is represented in three-dimensions. Instabilities emerge that regulate the strength of the pycnocline and coexist with persistent Ekman rolls, which are identified prior to the flow becoming intermittently unstable. When resolution of the z-level model is degraded to understand the grid-scale dependencies, the degradation is dominated by the established problem of excessive numerical diffusion. We show that at intermediate resolutions (2-4 m), the boundary layer structure can be partially recovered by tuning diffusivities. Lastly, we compare replacing prescribed melting with interactive melting that is dependent on the local ocean conditions. Interactive melting results in a feedback such that the system evolves more slowly, which is exaggerated at lower resolution. |
format |
Article in Journal/Newspaper |
author |
Patmore, Ryan D. Holland, Paul R. Vreugdenhil, Catherine A. Jenkins, Adrian Taylor, John R. |
spellingShingle |
Patmore, Ryan D. Holland, Paul R. Vreugdenhil, Catherine A. Jenkins, Adrian Taylor, John R. Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
author_facet |
Patmore, Ryan D. Holland, Paul R. Vreugdenhil, Catherine A. Jenkins, Adrian Taylor, John R. |
author_sort |
Patmore, Ryan D. |
title |
Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
title_short |
Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
title_full |
Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
title_fullStr |
Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
title_full_unstemmed |
Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
title_sort |
turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution |
publisher |
American Meteorological Society |
publishDate |
2023 |
url |
https://centaur.reading.ac.uk/108923/ https://centaur.reading.ac.uk/108923/1/1520-0485-JPO-D-22-0034.1.pdf |
genre |
Ice Shelf |
genre_facet |
Ice Shelf |
op_relation |
https://centaur.reading.ac.uk/108923/1/1520-0485-JPO-D-22-0034.1.pdf Patmore, Ryan D. ORCID logoorcid:0000-0002-5571-9229 , Holland, Paul R., Vreugdenhil, Catherine A., Jenkins, Adrian and Taylor, John R. (2023) Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution. Journal of Physical Oceanography, 53 (2). pp. 613-633. ISSN 1520-0485 doi: https://doi.org/10.1175/jpo-d-22-0034.1 <https://doi.org/10.1175/jpo-d-22-0034.1> |
op_rights |
cc_by_4 |
op_doi |
https://doi.org/10.1175/jpo-d-22-0034.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
53 |
container_issue |
2 |
container_start_page |
613 |
op_container_end_page |
633 |
_version_ |
1776201031666892800 |