Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study

A one-dimensional coupled sea ice–ocean model is used to investigate how the Arctic Ocean stratification and sea ice respond to changes in meltwater. In the control experiments, the model is capable of accurately simulating seasonal changes in the upper-ocean stratification structure compared with o...

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Published in:Ocean Science
Main Authors: Zhang, Haohao, Bai, Xuezhi, Wang, Kaiwen
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/os-19-1649-2023
https://os.copernicus.org/articles/19/1649/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:os110200 2023-12-31T10:03:19+01:00 Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study Zhang, Haohao Bai, Xuezhi Wang, Kaiwen 2023-11-29 application/pdf https://doi.org/10.5194/os-19-1649-2023 https://os.copernicus.org/articles/19/1649/2023/ eng eng doi:10.5194/os-19-1649-2023 https://os.copernicus.org/articles/19/1649/2023/ eISSN: 1812-0792 Text 2023 ftcopernicus https://doi.org/10.5194/os-19-1649-2023 2023-12-04T17:24:16Z A one-dimensional coupled sea ice–ocean model is used to investigate how the Arctic Ocean stratification and sea ice respond to changes in meltwater. In the control experiments, the model is capable of accurately simulating seasonal changes in the upper-ocean stratification structure compared with observations, and the results suggest that ocean stratification is important for ice thickness development during the freezing season. The sensitivity experiments reveal the following: (1) a decrease in meltwater release weakens ocean stratification and creates a deeper, higher-salinity mixed layer. (2) Meltwater reduced ice melting by 17 % by strengthening ocean stratification. (3) The impact of meltwater released during the previous melting season on ice growth in winter depends on the strength of stratification. After removing all the meltwater during the summer, ice formation in areas with strong stratification increased by 12 % during the winter, while it decreased by 43 % in areas with weak stratification. (4) In some areas of the Nansen Basin where stratification is nearly absent, the warm Atlantic Water can reach the ice directly in early spring, leading to early melting of the sea ice in winter if all meltwater is removed from the model. These findings contribute to our understanding of the complex interactions between ocean stratification, meltwater and sea ice growth and have important implications for climate models and future change prediction in the Arctic. Text Arctic Arctic Ocean Nansen Basin Sea ice Copernicus Publications: E-Journals Ocean Science 19 6 1649 1668
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A one-dimensional coupled sea ice–ocean model is used to investigate how the Arctic Ocean stratification and sea ice respond to changes in meltwater. In the control experiments, the model is capable of accurately simulating seasonal changes in the upper-ocean stratification structure compared with observations, and the results suggest that ocean stratification is important for ice thickness development during the freezing season. The sensitivity experiments reveal the following: (1) a decrease in meltwater release weakens ocean stratification and creates a deeper, higher-salinity mixed layer. (2) Meltwater reduced ice melting by 17 % by strengthening ocean stratification. (3) The impact of meltwater released during the previous melting season on ice growth in winter depends on the strength of stratification. After removing all the meltwater during the summer, ice formation in areas with strong stratification increased by 12 % during the winter, while it decreased by 43 % in areas with weak stratification. (4) In some areas of the Nansen Basin where stratification is nearly absent, the warm Atlantic Water can reach the ice directly in early spring, leading to early melting of the sea ice in winter if all meltwater is removed from the model. These findings contribute to our understanding of the complex interactions between ocean stratification, meltwater and sea ice growth and have important implications for climate models and future change prediction in the Arctic.
format Text
author Zhang, Haohao
Bai, Xuezhi
Wang, Kaiwen
spellingShingle Zhang, Haohao
Bai, Xuezhi
Wang, Kaiwen
Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
author_facet Zhang, Haohao
Bai, Xuezhi
Wang, Kaiwen
author_sort Zhang, Haohao
title Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
title_short Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
title_full Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
title_fullStr Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
title_full_unstemmed Response of the Arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
title_sort response of the arctic sea ice–ocean system to meltwater perturbations based on a one-dimensional model study
publishDate 2023
url https://doi.org/10.5194/os-19-1649-2023
https://os.copernicus.org/articles/19/1649/2023/
genre Arctic
Arctic Ocean
Nansen Basin
Sea ice
genre_facet Arctic
Arctic Ocean
Nansen Basin
Sea ice
op_source eISSN: 1812-0792
op_relation doi:10.5194/os-19-1649-2023
https://os.copernicus.org/articles/19/1649/2023/
op_doi https://doi.org/10.5194/os-19-1649-2023
container_title Ocean Science
container_volume 19
container_issue 6
container_start_page 1649
op_container_end_page 1668
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