Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean
Satellite-based observations and a pan-Arctic coupled sea ice-ocean model are utilized to study the effect of ocean geostrophic currents on large-scale sea ice circulation in the Canada Basin, Arctic Ocean. We find that surface winds primarily drive sea ice drifts in the west–east direction, while t...
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IOP Publishing
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Online Access: | https://doi.org/10.1088/1748-9326/ad6baa https://doaj.org/article/2e5ad8fe632a40c5a44ecf460ad83024 |
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ftdoajarticles:oai:doaj.org/article:2e5ad8fe632a40c5a44ecf460ad83024 2024-09-15T17:53:13+00:00 Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean Hengling Leng Hailun He Dake Chen Peigen Lin Yang Yang Zhaomin Wang 2024-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/ad6baa https://doaj.org/article/2e5ad8fe632a40c5a44ecf460ad83024 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/ad6baa https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ad6baa 1748-9326 https://doaj.org/article/2e5ad8fe632a40c5a44ecf460ad83024 Environmental Research Letters, Vol 19, Iss 9, p 094040 (2024) geostrophic currents sea ice circulation Arctic Ocean Beaufort Gyre Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2024 ftdoajarticles https://doi.org/10.1088/1748-9326/ad6baa 2024-08-19T14:56:38Z Satellite-based observations and a pan-Arctic coupled sea ice-ocean model are utilized to study the effect of ocean geostrophic currents on large-scale sea ice circulation in the Canada Basin, Arctic Ocean. We find that surface winds primarily drive sea ice drifts in the west–east direction, while the geostrophic currents in the Beaufort Gyre promote north–south ice drifts. Wind fluctuations can create variable ice drifts, yet geostrophic currents respond more slowly due to their larger vertical scale, serving as a slowly-evolving conveyor belt for maintaining the anticyclonic ice circulation. It is further demonstrated that the bathymetry can regulate the movement of sea ice via constraining the expansion of ocean circulation. This mechanism is indirect in the sense that the ice is far from the seafloor. Our research underscores the necessity of considering the bathymetry-constrained geostrophic currents in understanding Arctic sea ice dynamics. With the rapid retreat of Arctic sea ice, the multi-scale interactions between ice drifts and ocean currents may have significant implications for the Arctic ecosystem, climate, and shipping corridors. Article in Journal/Newspaper Arctic Ocean canada basin Sea ice Directory of Open Access Journals: DOAJ Articles Environmental Research Letters 19 9 094040 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
geostrophic currents sea ice circulation Arctic Ocean Beaufort Gyre Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
geostrophic currents sea ice circulation Arctic Ocean Beaufort Gyre Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Hengling Leng Hailun He Dake Chen Peigen Lin Yang Yang Zhaomin Wang Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
topic_facet |
geostrophic currents sea ice circulation Arctic Ocean Beaufort Gyre Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
Satellite-based observations and a pan-Arctic coupled sea ice-ocean model are utilized to study the effect of ocean geostrophic currents on large-scale sea ice circulation in the Canada Basin, Arctic Ocean. We find that surface winds primarily drive sea ice drifts in the west–east direction, while the geostrophic currents in the Beaufort Gyre promote north–south ice drifts. Wind fluctuations can create variable ice drifts, yet geostrophic currents respond more slowly due to their larger vertical scale, serving as a slowly-evolving conveyor belt for maintaining the anticyclonic ice circulation. It is further demonstrated that the bathymetry can regulate the movement of sea ice via constraining the expansion of ocean circulation. This mechanism is indirect in the sense that the ice is far from the seafloor. Our research underscores the necessity of considering the bathymetry-constrained geostrophic currents in understanding Arctic sea ice dynamics. With the rapid retreat of Arctic sea ice, the multi-scale interactions between ice drifts and ocean currents may have significant implications for the Arctic ecosystem, climate, and shipping corridors. |
format |
Article in Journal/Newspaper |
author |
Hengling Leng Hailun He Dake Chen Peigen Lin Yang Yang Zhaomin Wang |
author_facet |
Hengling Leng Hailun He Dake Chen Peigen Lin Yang Yang Zhaomin Wang |
author_sort |
Hengling Leng |
title |
Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
title_short |
Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
title_full |
Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
title_fullStr |
Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
title_full_unstemmed |
Bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the Canada Basin, Arctic Ocean |
title_sort |
bathymetry-constrained ocean geostrophic currents play a key role in shaping the sea ice circulation in the canada basin, arctic ocean |
publisher |
IOP Publishing |
publishDate |
2024 |
url |
https://doi.org/10.1088/1748-9326/ad6baa https://doaj.org/article/2e5ad8fe632a40c5a44ecf460ad83024 |
genre |
Arctic Ocean canada basin Sea ice |
genre_facet |
Arctic Ocean canada basin Sea ice |
op_source |
Environmental Research Letters, Vol 19, Iss 9, p 094040 (2024) |
op_relation |
https://doi.org/10.1088/1748-9326/ad6baa https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ad6baa 1748-9326 https://doaj.org/article/2e5ad8fe632a40c5a44ecf460ad83024 |
op_doi |
https://doi.org/10.1088/1748-9326/ad6baa |
container_title |
Environmental Research Letters |
container_volume |
19 |
container_issue |
9 |
container_start_page |
094040 |
_version_ |
1810295235134095360 |