Factors affecting the subsurface aragonite undersaturation layer in the Pacific Arctic region
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Mo, Ahra | - |
dc.contributor.author | Kim, Dongseon | - |
dc.contributor.author | Yang, Eun Jin | - |
dc.contributor.author | Jung, Jinyoung | - |
dc.contributor.author | Ko, Young Ho | - |
dc.contributor.author | Kang, Sung-Ho | - |
dc.contributor.author | Cho, Kyoung-Ho | - |
dc.contributor.author | Park, Keyhong | - |
dc.contributor.author | Kim, Tae-Wook | - |
dc.date.accessioned | 2022-09-23T08:40:31Z | - |
dc.date.available | 2022-09-23T08:40:31Z | - |
dc.date.created | 2022-09-23 | - |
dc.date.issued | 2022-10 | - |
dc.identifier.issn | 0025-326X | - |
dc.identifier.uri | https://scholar.korea.ac.kr/handle/2021.sw.korea/143728 | - |
dc.description.abstract | This study evaluated interannual variation in the subsurface aragonite undersaturation zone (omega Ar<1 layer) in the Pacific Arctic Ocean, using data from the 2016-2019 period. The upper boundary (DEP omega<1UB ) of the omega Ar<1 layer generally formed at a depth where the contribution of corrosive Pacific water was approximately 98 %. The intensity of the Beaufort Gyre associated with freshwater accumulation mainly determined interannual variation in DEP omega<1 UB , but the direction of its effect was opposite west and east of -166 degrees W. The lower boundary (DEP omega<1 LB ) of the omega Ar<1 layer was generally found at a depth range where equal contributions of Pacific and Atlantic water were expected. An Atlantic-origin cold saline water intrusion event in 2017 caused by an anomalous atmospheric circulation pattern significantly lifted the DEP omega<1LB , thus the thickness of the omega Ar<1 layer decreased. | - |
dc.language | English | - |
dc.language.iso | en | - |
dc.publisher | PERGAMON-ELSEVIER SCIENCE LTD | - |
dc.subject | SEA-ICE DECLINE | - |
dc.subject | OCEAN ACIDIFICATION | - |
dc.subject | FRESH-WATER | - |
dc.subject | BEAUFORT GYRE | - |
dc.subject | ANTHROPOGENIC CO2 | - |
dc.subject | CANADIAN BASIN | - |
dc.subject | SHELF WATERS | - |
dc.subject | ATLANTIC | - |
dc.subject | CARBON | - |
dc.subject | CIRCULATION | - |
dc.title | Factors affecting the subsurface aragonite undersaturation layer in the Pacific Arctic region | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Kim, Tae-Wook | - |
dc.identifier.doi | 10.1016/j.marpolbul.2022.114060 | - |
dc.identifier.scopusid | 2-s2.0-85136264952 | - |
dc.identifier.wosid | 000849961000002 | - |
dc.identifier.bibliographicCitation | MARINE POLLUTION BULLETIN, v.183 | - |
dc.relation.isPartOf | MARINE POLLUTION BULLETIN | - |
dc.citation.title | MARINE POLLUTION BULLETIN | - |
dc.citation.volume | 183 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Environmental Sciences & Ecology | - |
dc.relation.journalResearchArea | Marine & Freshwater Biology | - |
dc.relation.journalWebOfScienceCategory | Environmental Sciences | - |
dc.relation.journalWebOfScienceCategory | Marine & Freshwater Biology | - |
dc.subject.keywordPlus | ANTHROPOGENIC CO2 | - |
dc.subject.keywordPlus | ATLANTIC | - |
dc.subject.keywordPlus | BEAUFORT GYRE | - |
dc.subject.keywordPlus | CANADIAN BASIN | - |
dc.subject.keywordPlus | CARBON | - |
dc.subject.keywordPlus | CIRCULATION | - |
dc.subject.keywordPlus | FRESH-WATER | - |
dc.subject.keywordPlus | OCEAN ACIDIFICATION | - |
dc.subject.keywordPlus | SEA-ICE DECLINE | - |
dc.subject.keywordPlus | SHELF WATERS | - |
dc.subject.keywordAuthor | Aragonite saturation | - |
dc.subject.keywordAuthor | Arctic Ocean | - |
dc.subject.keywordAuthor | Atmospheric circulation | - |
dc.subject.keywordAuthor | Beaufort gyre | - |
dc.subject.keywordAuthor | Ocean acidification | - |
dc.subject.keywordAuthor | Pacific -Arctic regions | - |
Items in ScholarWorks are protected by copyright, with all rights reserved, unless otherwise indicated.
(02841) 서울특별시 성북구 안암로 14502-3290-1114
COPYRIGHT © 2021 Korea University. All Rights Reserved.
Certain data included herein are derived from the © Web of Science of Clarivate Analytics. All rights reserved.
You may not copy or re-distribute this material in whole or in part without the prior written consent of Clarivate Analytics.