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作 者:Wenjian HUA Aiguo DAI
机构地区:[1]Key Laboratory of Meteorological Disaster,Ministry of Education/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Information Science and Technology,Nanjing 210044,China [2]Department of Atmospheric and Environmental Sciences,University at Albany,State University of New York,Albany 12222,USA
出 处:《Science China Earth Sciences》2024年第8期2699-2701,共3页中国科学(地球科学英文版)
基 金:supported by the National Key R&D Program of China(Grant No.2022YFF0801601);the National Natural Science Foundation of China(Grant No.42075022);supported by the U.S.National Science Foundation(Grant No.AGS-2015780)。
摘 要:The physical formation mechanisms of the Atlantic Multidecadal Variability(AMV)in the context of global warming have been a key research topic(Vecchi et al.,2017).The conventional view is that the AMV is mainly driven by internal dynamics within the climate system,especially in the Atlantic Ocean(Zhang et al.,2019).However,some studies suggest that decadal to multidecadal variations in North Atlantic sea surface temperature(SST)since around 1950 are related to anthropogenic and natural aerosol emissions(Otter?et al.,2010;Booth et al.,2012;Hua et al.,2019).
关 键 词:ATLANTIC DECADAL FORCING
分 类 号:P467[天文地球—大气科学及气象学] P73
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