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...

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Published in:Environmental Research Letters
Main Authors: Yujun Liu, Yijun He
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2023
Subjects:
Q
Online Access:https://doi.org/10.1088/1748-9326/ad0518
https://doaj.org/article/e7c5bc41e7944b7cb602d85aace1d1a3
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spelling 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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