Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone

Ocean heat exchanges at the marginal ice zone (MIZ) play an important role in melting sea ice. Mixed-layer eddies transport heat and ice floes across the MIZ, facilitating the pack's access to warm waters. This study explores these frontal dynamics using disk-shaped floes coupled to an upper-oc...

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Published in:Geophysical Research Letters
Main Authors: Gupta, Mukund, Gürcan, Emma, Thompson, Andrew F.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2024
Subjects:
Online Access:https://doi.org/10.1029/2023gl105656
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spelling ftcaltechauth:oai:authors.library.caltech.edu:gjb2k-sf521 2024-09-15T18:34:14+00:00 Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone Gupta, Mukund Gürcan, Emma Thompson, Andrew F. 2024-01-28 https://doi.org/10.1029/2023gl105656 eng eng American Geophysical Union https://doi.org/10.1029/2023gl105656 oai:authors.library.caltech.edu:gjb2k-sf521 issn:1944-8007 info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode Geophysical Research Letters, 51(2), e2023GL105656, (2024-01-28) info:eu-repo/semantics/article 2024 ftcaltechauth https://doi.org/10.1029/2023gl105656 2024-08-06T15:35:05Z Ocean heat exchanges at the marginal ice zone (MIZ) play an important role in melting sea ice. Mixed-layer eddies transport heat and ice floes across the MIZ, facilitating the pack's access to warm waters. This study explores these frontal dynamics using disk-shaped floes coupled to an upper-ocean model simulating the sea ice edge. Numerical experiments reveal that small floes respond more strongly to fine-scale ocean currents, which favors higher dispersion rates and weakens sea ice drag onto the underlying ocean. Floes with radii smaller than resolved turbulent filaments (∼2–4 km) result in a wider and more energetic MIZ, by a factor of 70% each, compared to larger floes. We hypothesize that this floe size dependency may affect sea ice break-up by controlling oceanic energy propagation into the MIZ and modulate the sea ice pack's melt rate by regulating lateral heat transport toward the sea ice cover. © 2024. The Authors. This is an open access article underthe terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. M.G., E.G., and A.F.T. were supported by the Office of Naval Research Multidisciplinary University Research Initiative (MURI) on Mathematics and Data Science for Physical Modeling and Prediction of Sea Ice. A.F.T. also acknowledges support from the NSF OCE 1829969 Grant. The authors are grateful to two anonymous reviewers, whose insightful comments helped improve the manuscript. Conceptualization: Mukund Gupta, Andrew F. Thompson Formal analysis: Mukund Gupta, Emma Gürcan Funding acquisition: Andrew F. Thompson Investigation: Mukund Gupta, Andrew F. Thompson Methodology: Mukund Gupta Project Administration: Andrew F. Thompson Resources: Andrew F. Thompson Software: Mukund Gupta Supervision: Mukund Gupta, Andrew F. Thompson Validation: Mukund Gupta The sea ice floe code is provided in Gupta(2022), ... Article in Journal/Newspaper Sea ice Caltech Authors (California Institute of Technology) Geophysical Research Letters 51 2
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language English
description Ocean heat exchanges at the marginal ice zone (MIZ) play an important role in melting sea ice. Mixed-layer eddies transport heat and ice floes across the MIZ, facilitating the pack's access to warm waters. This study explores these frontal dynamics using disk-shaped floes coupled to an upper-ocean model simulating the sea ice edge. Numerical experiments reveal that small floes respond more strongly to fine-scale ocean currents, which favors higher dispersion rates and weakens sea ice drag onto the underlying ocean. Floes with radii smaller than resolved turbulent filaments (∼2–4 km) result in a wider and more energetic MIZ, by a factor of 70% each, compared to larger floes. We hypothesize that this floe size dependency may affect sea ice break-up by controlling oceanic energy propagation into the MIZ and modulate the sea ice pack's melt rate by regulating lateral heat transport toward the sea ice cover. © 2024. The Authors. This is an open access article underthe terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. M.G., E.G., and A.F.T. were supported by the Office of Naval Research Multidisciplinary University Research Initiative (MURI) on Mathematics and Data Science for Physical Modeling and Prediction of Sea Ice. A.F.T. also acknowledges support from the NSF OCE 1829969 Grant. The authors are grateful to two anonymous reviewers, whose insightful comments helped improve the manuscript. Conceptualization: Mukund Gupta, Andrew F. Thompson Formal analysis: Mukund Gupta, Emma Gürcan Funding acquisition: Andrew F. Thompson Investigation: Mukund Gupta, Andrew F. Thompson Methodology: Mukund Gupta Project Administration: Andrew F. Thompson Resources: Andrew F. Thompson Software: Mukund Gupta Supervision: Mukund Gupta, Andrew F. Thompson Validation: Mukund Gupta The sea ice floe code is provided in Gupta(2022), ...
format Article in Journal/Newspaper
author Gupta, Mukund
Gürcan, Emma
Thompson, Andrew F.
spellingShingle Gupta, Mukund
Gürcan, Emma
Thompson, Andrew F.
Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
author_facet Gupta, Mukund
Gürcan, Emma
Thompson, Andrew F.
author_sort Gupta, Mukund
title Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_short Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_full Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_fullStr Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_full_unstemmed Eddyâ€Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_sort eddyâ€induced dispersion of sea ice floes at the marginal ice zone
publisher American Geophysical Union
publishDate 2024
url https://doi.org/10.1029/2023gl105656
genre Sea ice
genre_facet Sea ice
op_source Geophysical Research Letters, 51(2), e2023GL105656, (2024-01-28)
op_relation https://doi.org/10.1029/2023gl105656
oai:authors.library.caltech.edu:gjb2k-sf521
issn:1944-8007
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
op_doi https://doi.org/10.1029/2023gl105656
container_title Geophysical Research Letters
container_volume 51
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