Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean

Storms can have a direct impact on sea ice, but whether their effect is seen weeks to months later has received little attention. The immediate and longer term impacts of an idealized open water wind storm are investigated with a one-dimensional coupled ice-ocean model. Storms with different momentu...

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Main Authors: Bent, Emma, Lique, Camille, Sutherland, Peter
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
Subjects:
Online Access:http://dx.doi.org/10.22541/essoar.170016444.45417778/v1
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spelling crwinnower:10.22541/essoar.170016444.45417778/v1 2024-06-02T08:02:34+00:00 Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean Bent, Emma Lique, Camille Sutherland, Peter 2023 http://dx.doi.org/10.22541/essoar.170016444.45417778/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.170016444.45417778/v1 2024-05-07T14:19:21Z Storms can have a direct impact on sea ice, but whether their effect is seen weeks to months later has received little attention. The immediate and longer term impacts of an idealized open water wind storm are investigated with a one-dimensional coupled ice-ocean model. Storms with different momentum, duration and date of occurrence are tested. During the storm, the mechanical forcing causes a deepening of the mixed layer, leading to an increase in mixed layer heat content, despite a decrease in mixed layer temperature. This results in a delay in sea ice formation that ranges between a few hours to weeks compared to the control run, depending on the storm characteristics. Throughout the freezing period, the storm-induced thick mixed layer experiences little variability, preventing warm water entrainment at the base of the mixed layer. This leads to faster sea ice growth compared to the control run, resulting in sea ice thickness differences of a few millimeters to around 10 cm before the melting onset. These results are stronger for runs with higher momentum storms which cause greater mixed layer deepening. Storms occurring in early August, when the ocean surface heat flux is positive, also amplify the results by forcing a greater increase in mixed layer heat content. The impacts of the storms are sensitive to the initial stratification, and amplified for a highly stratified ocean. We suggest that localized storms could significantly influence the seasonal dynamics of the mixed layer and consequently impact sea ice conditions. Other/Unknown Material Arctic Arctic Ocean Sea ice The Winnower Arctic Arctic Ocean
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description Storms can have a direct impact on sea ice, but whether their effect is seen weeks to months later has received little attention. The immediate and longer term impacts of an idealized open water wind storm are investigated with a one-dimensional coupled ice-ocean model. Storms with different momentum, duration and date of occurrence are tested. During the storm, the mechanical forcing causes a deepening of the mixed layer, leading to an increase in mixed layer heat content, despite a decrease in mixed layer temperature. This results in a delay in sea ice formation that ranges between a few hours to weeks compared to the control run, depending on the storm characteristics. Throughout the freezing period, the storm-induced thick mixed layer experiences little variability, preventing warm water entrainment at the base of the mixed layer. This leads to faster sea ice growth compared to the control run, resulting in sea ice thickness differences of a few millimeters to around 10 cm before the melting onset. These results are stronger for runs with higher momentum storms which cause greater mixed layer deepening. Storms occurring in early August, when the ocean surface heat flux is positive, also amplify the results by forcing a greater increase in mixed layer heat content. The impacts of the storms are sensitive to the initial stratification, and amplified for a highly stratified ocean. We suggest that localized storms could significantly influence the seasonal dynamics of the mixed layer and consequently impact sea ice conditions.
format Other/Unknown Material
author Bent, Emma
Lique, Camille
Sutherland, Peter
spellingShingle Bent, Emma
Lique, Camille
Sutherland, Peter
Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
author_facet Bent, Emma
Lique, Camille
Sutherland, Peter
author_sort Bent, Emma
title Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
title_short Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
title_full Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
title_fullStr Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
title_full_unstemmed Impact of an isolated open water storm on sea ice and ocean conditions in the Arctic Ocean
title_sort impact of an isolated open water storm on sea ice and ocean conditions in the arctic ocean
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.170016444.45417778/v1
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_doi https://doi.org/10.22541/essoar.170016444.45417778/v1
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