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Frequent central Pacific La Nina events may accelerate Arctic warming since the 1980s

Frequent central Pacific La Ni?a events may accelerate Arctic warming since the 1980s

作     者:Jing Li Lin Mu Linhao Zhong Jing Li;Lin Mu;Linhao Zhong

作者机构:College of Life Sciences and OceanographyShenzhen UniversityShenzhen 518060China College of Marine Science and TechnologyChina University of GeosciencesWuhan 430074China Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)Guangzhou 511458China CAS Key Laboratory of Regional Climate-Environment for Temperate East AsiaInstitute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China 

出 版 物:《Acta Oceanologica Sinica》 (海洋学报(英文版))

年 卷 期:2021年第40卷第11期

页      面:62-69页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 070601[理学-气象学] 0706[理学-大气科学] 

基  金:The Shenzhen Fundamental Research Program under contract No.JCYJ20200109110220482 the National Natural Science Foundation of China under contract No.U2006210 the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)under contract No.GML2019ZD0604 

主  题:ENSO diversity La Nina type the Arctic warming 

摘      要:Including significant warming trend,Arctic climate changes also exhibit strong interannual variations in various fields,which is suggested to be related to El Nino and Southern Oscillation(ENSO)*** studies have demonstrated the different impacts on the Arctic of central Pacific(CP)and eastern Pacific(EP)ENSO events,and suggested these impacts are largely of opposite sign for ENSO warm and cold *** results illustrate asymmetrical changes for the cold and warm ENSO events,especially for the La Nina *** to the past frequent basin-wide cooling La Nina events,since the 1980 s the cooling center for the La Nina event has strengthened and moved westward along with the increasing frequency for the canonical and CP La Nina *** to the basin-wide cooling and canonical La Nina events,the frequent CP La Nina events induce significant warming from the Beaufort Sea to Greenland via the convection center moving northward over the western *** analysis and numerical experiments both suggest that the changes in La Nina type may also accelerate Arctic warming.

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