How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas?
Arctic warming over the Barents–Kara Seas and its impacts on the mid-latitude circulations have been widely discussed. However, the specific mechanism that brings the warming still remains unclear. In this study, a possible cause of the regional Arctic warming over the Barents–Kara Seas during early...
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Online Access: | https://doi.org/10.1088/1748-9326/aa5f3b https://doaj.org/article/7dfa5e7305a6434b92cbdbb3c5131bbc |
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ftdoajarticles:oai:doaj.org/article:7dfa5e7305a6434b92cbdbb3c5131bbc 2023-09-05T13:16:20+02:00 How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? Ok Jung Mi-Kyung Sung Kazutoshi Sato Young-Kwon Lim Seong-Joong Kim Eun-Hyuk Baek Jee-Hoon Jeong Baek-Min Kim 2017-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aa5f3b https://doaj.org/article/7dfa5e7305a6434b92cbdbb3c5131bbc EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aa5f3b https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aa5f3b 1748-9326 https://doaj.org/article/7dfa5e7305a6434b92cbdbb3c5131bbc Environmental Research Letters, Vol 12, Iss 3, p 034021 (2017) Arctic warming Stationary Wave Model transient eddy vorticity forcing Western North Atlantic Ocean Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2017 ftdoajarticles https://doi.org/10.1088/1748-9326/aa5f3b 2023-08-13T00:37:40Z Arctic warming over the Barents–Kara Seas and its impacts on the mid-latitude circulations have been widely discussed. However, the specific mechanism that brings the warming still remains unclear. In this study, a possible cause of the regional Arctic warming over the Barents–Kara Seas during early winter (October–December) is suggested. We found that warmer sea surface temperature anomalies over the western North Atlantic Ocean (WNAO) modulate the transient eddies overlying the oceanic frontal region. The altered transient eddy vorticity flux acts as a source for the Rossby wave straddling the western North Atlantic and the Barents–Kara Seas (Scandinavian pattern), and induces a significant warm advection, increasing surface and lower-level temperature over the Eurasian sector of the Arctic Ocean. The importance of the sea surface temperature anomalies over the WNAO and subsequent transient eddy forcing over the WNAO was also supported by both specially designed simple model experiments and general circulation model experiments. Article in Journal/Newspaper Arctic Arctic Ocean North Atlantic Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Environmental Research Letters 12 3 034021 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic warming Stationary Wave Model transient eddy vorticity forcing Western North Atlantic Ocean Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
Arctic warming Stationary Wave Model transient eddy vorticity forcing Western North Atlantic Ocean Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Ok Jung Mi-Kyung Sung Kazutoshi Sato Young-Kwon Lim Seong-Joong Kim Eun-Hyuk Baek Jee-Hoon Jeong Baek-Min Kim How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
topic_facet |
Arctic warming Stationary Wave Model transient eddy vorticity forcing Western North Atlantic Ocean Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
Arctic warming over the Barents–Kara Seas and its impacts on the mid-latitude circulations have been widely discussed. However, the specific mechanism that brings the warming still remains unclear. In this study, a possible cause of the regional Arctic warming over the Barents–Kara Seas during early winter (October–December) is suggested. We found that warmer sea surface temperature anomalies over the western North Atlantic Ocean (WNAO) modulate the transient eddies overlying the oceanic frontal region. The altered transient eddy vorticity flux acts as a source for the Rossby wave straddling the western North Atlantic and the Barents–Kara Seas (Scandinavian pattern), and induces a significant warm advection, increasing surface and lower-level temperature over the Eurasian sector of the Arctic Ocean. The importance of the sea surface temperature anomalies over the WNAO and subsequent transient eddy forcing over the WNAO was also supported by both specially designed simple model experiments and general circulation model experiments. |
format |
Article in Journal/Newspaper |
author |
Ok Jung Mi-Kyung Sung Kazutoshi Sato Young-Kwon Lim Seong-Joong Kim Eun-Hyuk Baek Jee-Hoon Jeong Baek-Min Kim |
author_facet |
Ok Jung Mi-Kyung Sung Kazutoshi Sato Young-Kwon Lim Seong-Joong Kim Eun-Hyuk Baek Jee-Hoon Jeong Baek-Min Kim |
author_sort |
Ok Jung |
title |
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
title_short |
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
title_full |
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
title_fullStr |
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
title_full_unstemmed |
How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents–Kara Seas? |
title_sort |
how does the sst variability over the western north atlantic ocean control arctic warming over the barents–kara seas? |
publisher |
IOP Publishing |
publishDate |
2017 |
url |
https://doi.org/10.1088/1748-9326/aa5f3b https://doaj.org/article/7dfa5e7305a6434b92cbdbb3c5131bbc |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean North Atlantic |
genre_facet |
Arctic Arctic Ocean North Atlantic |
op_source |
Environmental Research Letters, Vol 12, Iss 3, p 034021 (2017) |
op_relation |
https://doi.org/10.1088/1748-9326/aa5f3b https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aa5f3b 1748-9326 https://doaj.org/article/7dfa5e7305a6434b92cbdbb3c5131bbc |
op_doi |
https://doi.org/10.1088/1748-9326/aa5f3b |
container_title |
Environmental Research Letters |
container_volume |
12 |
container_issue |
3 |
container_start_page |
034021 |
_version_ |
1776197967505522688 |