Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean
In recent years, as the Arctic Ocean’s warming trend has accelerated, there has been increasing attention on the process of Atlantification in the Arctic Ocean. This study focused on the Arctic Atlantic inflow zone (AAZ) as its research area. Multi-source reanalysis data and in-situ Argo float data...
Published in: | Environmental Research Letters |
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Online Access: | https://doi.org/10.1088/1748-9326/ad0518 https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3 |
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ftdoajarticles:oai:doaj.org/article:e7c5bc41e7944b7cb602d85aace1d1a3 2023-12-03T10:15:41+01:00 Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean Yujun Liu Yijun He 2023-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/ad0518 https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/ad0518 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ad0518 1748-9326 https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3 Environmental Research Letters, Vol 18, Iss 11, p 114049 (2023) Arctic strong cyclone Arctic Ocean Atlantification ocean heat content Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2023 ftdoajarticles https://doi.org/10.1088/1748-9326/ad0518 2023-11-05T01:41:56Z In recent years, as the Arctic Ocean’s warming trend has accelerated, there has been increasing attention on the process of Atlantification in the Arctic Ocean. This study focused on the Arctic Atlantic inflow zone (AAZ) as its research area. Multi-source reanalysis data and in-situ Argo float data were utilized to detect Arctic strong cyclones (ASCs) in the AAZ and analyze the resulting changes in the upper ocean. The findings reveal that during the cold season (October to March), influenced by ASCs’ intensity, frequency, tracks, and the concurrent weakening of ocean stratification, these cyclones can disrupt the cold halocline layer through mechanisms such as mixing and Ekman pumping. This process facilitates the transport of heat from the deep, warm and saline Atlantic Water within the ocean to the subsurface layers. Concurrently, ASCs during the cold season can enhance the process of Atlantification in the Arctic Ocean by intensifying the intrusion of the Barents Sea Branch. Additionally, the attenuation of oceanic stratification during ASCs is primarily driven by changes in salinity, particularly above the 100 m. Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Barents Sea Environmental Research Letters 18 11 114049 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic strong cyclone Arctic Ocean Atlantification ocean heat content Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
Arctic strong cyclone Arctic Ocean Atlantification ocean heat content Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Yujun Liu Yijun He Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
topic_facet |
Arctic strong cyclone Arctic Ocean Atlantification ocean heat content Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
In recent years, as the Arctic Ocean’s warming trend has accelerated, there has been increasing attention on the process of Atlantification in the Arctic Ocean. This study focused on the Arctic Atlantic inflow zone (AAZ) as its research area. Multi-source reanalysis data and in-situ Argo float data were utilized to detect Arctic strong cyclones (ASCs) in the AAZ and analyze the resulting changes in the upper ocean. The findings reveal that during the cold season (October to March), influenced by ASCs’ intensity, frequency, tracks, and the concurrent weakening of ocean stratification, these cyclones can disrupt the cold halocline layer through mechanisms such as mixing and Ekman pumping. This process facilitates the transport of heat from the deep, warm and saline Atlantic Water within the ocean to the subsurface layers. Concurrently, ASCs during the cold season can enhance the process of Atlantification in the Arctic Ocean by intensifying the intrusion of the Barents Sea Branch. Additionally, the attenuation of oceanic stratification during ASCs is primarily driven by changes in salinity, particularly above the 100 m. |
format |
Article in Journal/Newspaper |
author |
Yujun Liu Yijun He |
author_facet |
Yujun Liu Yijun He |
author_sort |
Yujun Liu |
title |
Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
title_short |
Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
title_full |
Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
title_fullStr |
Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
title_full_unstemmed |
Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
title_sort |
cold season arctic strong cyclones enhance atlantification of the arctic ocean |
publisher |
IOP Publishing |
publishDate |
2023 |
url |
https://doi.org/10.1088/1748-9326/ad0518 https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3 |
geographic |
Arctic Arctic Ocean Barents Sea |
geographic_facet |
Arctic Arctic Ocean Barents Sea |
genre |
Arctic Arctic Ocean Barents Sea |
genre_facet |
Arctic Arctic Ocean Barents Sea |
op_source |
Environmental Research Letters, Vol 18, Iss 11, p 114049 (2023) |
op_relation |
https://doi.org/10.1088/1748-9326/ad0518 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ad0518 1748-9326 https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3 |
op_doi |
https://doi.org/10.1088/1748-9326/ad0518 |
container_title |
Environmental Research Letters |
container_volume |
18 |
container_issue |
11 |
container_start_page |
114049 |
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1784262563594240000 |