Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone

Abstract 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...

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Main Authors: Mukund Gupta, Emma Gürcan, Andrew F. Thompson
Format: Article
Language:English
Published: Wiley 2024-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL105656
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author Mukund Gupta
Emma Gürcan
Andrew F. Thompson
author_facet Mukund Gupta
Emma Gürcan
Andrew F. Thompson
author_sort Mukund Gupta
collection DOAJ
description Abstract 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.
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spelling doaj-art-ca7d782d4f2c45bd983ef86eb3a1cb5c2025-08-20T02:11:09ZengWileyGeophysical Research Letters0094-82761944-80072024-01-01512n/an/a10.1029/2023GL105656Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice ZoneMukund Gupta0Emma Gürcan1Andrew F. Thompson2California Institute of Technology Pasadena CA USACalifornia Institute of Technology Pasadena CA USACalifornia Institute of Technology Pasadena CA USAAbstract 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.https://doi.org/10.1029/2023GL105656sea iceoceanographypolar climateeddiessubmesoscaleheat transport
spellingShingle Mukund Gupta
Emma Gürcan
Andrew F. Thompson
Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
Geophysical Research Letters
sea ice
oceanography
polar climate
eddies
submesoscale
heat transport
title Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_full Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_fullStr Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_full_unstemmed Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_short Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone
title_sort eddy induced dispersion of sea ice floes at the marginal ice zone
topic sea ice
oceanography
polar climate
eddies
submesoscale
heat transport
url https://doi.org/10.1029/2023GL105656
work_keys_str_mv AT mukundgupta eddyinduceddispersionofseaicefloesatthemarginalicezone
AT emmagurcan eddyinduceddispersionofseaicefloesatthemarginalicezone
AT andrewfthompson eddyinduceddispersionofseaicefloesatthemarginalicezone