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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| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
IOP Publishing
2023-01-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1088/1748-9326/ad0518 |
| _version_ | 1851915743925370880 |
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| author | Yujun Liu Yijun He |
| author_facet | Yujun Liu Yijun He |
| author_sort | Yujun Liu |
| collection | DOAJ |
| container_title | Environmental Research Letters |
| 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 |
| id | doaj-art-e7c5bc41e7944b7cb602d85aace1d1a3 |
| institution | Directory of Open Access Journals |
| issn | 1748-9326 |
| language | English |
| publishDate | 2023-01-01 |
| publisher | IOP Publishing |
| record_format | Article |
| spelling | doaj-art-e7c5bc41e7944b7cb602d85aace1d1a32025-08-19T22:00:12ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-01181111404910.1088/1748-9326/ad0518Cold season Arctic strong cyclones enhance Atlantification of the Arctic OceanYujun Liu0https://orcid.org/0000-0003-3438-9870Yijun He1https://orcid.org/0000-0002-1531-5262School of Marine Sciences, Nanjing University of Information Science and Technology , Nanjing 210044, People’s Republic of ChinaSchool of Marine Sciences, Nanjing University of Information Science and Technology , Nanjing 210044, People’s Republic of China; Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology , Qingdao 266237, People’s Republic of China; Key Laboratory of Space Ocean Remote Sensing and Applications, National Satellite Ocean Application Service , Beijing 100081, People’s Republic of ChinaIn 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.https://doi.org/10.1088/1748-9326/ad0518Arctic strong cycloneArctic OceanAtlantificationocean heat content |
| spellingShingle | Yujun Liu Yijun He Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean Arctic strong cyclone Arctic Ocean Atlantification ocean heat content |
| title | 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_short | Cold season Arctic strong cyclones enhance Atlantification of the Arctic Ocean |
| title_sort | cold season arctic strong cyclones enhance atlantification of the arctic ocean |
| topic | Arctic strong cyclone Arctic Ocean Atlantification ocean heat content |
| url | https://doi.org/10.1088/1748-9326/ad0518 |
| work_keys_str_mv | AT yujunliu coldseasonarcticstrongcyclonesenhanceatlantificationofthearcticocean AT yijunhe coldseasonarcticstrongcyclonesenhanceatlantificationofthearcticocean |
