首站-论文投稿智能助手
典型文献
Asian summer monsoon responses to the change of land-sea thermodynamic contrast in a warming climate:CMIP6 projections
文献摘要:
It is of practical significance to use the updated Coupled Model Intercomparison Project Phase 6(CMIP6)models to study the impact of changes in land-sea thermodynamic contrast(TC)on the Asian summer monsoon under different scenarios and to compare the similarities and differences of the impact mechanisms between different monsoon regions.In this study,we investigated future changes of the Asian summer monsoon under four Shared Socioeconomic Pathway(SSP)scenarios using 19 CMIP6 models.The intensity of the South Asian summer monsoon(SASM)is projected to decrease by 2.6%,6.3%,10.1%,and 11.1%,while the East Asian summer monsoon(EASM)intensity is projected to increase by 4.6%,7.9%,7.4%,and 9.8%until the end of the 21st century for SSP126,SSP245,SSP370,and SSP585 scenarios,respectively.Moreover,summer precipitation in Asia is projected to increase remarkably in 2015-2099 under all four scenarios.The incon-sistent warming trends over the Tibetan Plateau(TP),Northwest Pacific,and tropical Indian Ocean would greatly impact the monsoon cir-culations.The upper-troposphere warming trend over the surrounding oceans is remarkably greater than that over the TP,while the near-surface warming trend over the surrounding oceans is smaller than that over the TP.The decrease of upper-troposphere TC between the TP and tropical Indian Ocean results in a weakening of the SASM circulation.The enhancement of the lower-troposphere TC between the TP and Northwest Pacific would strengthen the EASM circulation.Moisture budget analysis shows that the water-vapor would increase in the future,which would thermodynamically enhance summer precipitation through the anomalous vertical moisture transport associated with mean flow.The strengthening of the meridional circulation of the EASM would increase monsoon precipitation,while the weakening of zonal circulation of the SASM would dynamically reduce South Asian summer precipitation.
文献关键词:
作者姓名:
Qing-Yuan WU;Qing-Quan LI;Yi-Hui DING;Xin-Yong SHEN;Meng-Chu ZHAO;Yu-Xiang ZHU
作者机构:
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Key Laboratory of Meteorological Disaster Ministry of Education/Joint International Research Laboratory on Climate and Environment Change,Nanjing University of Information Science&Technology,Nanjing 210044,China;Laboratory for Climate Studies,National Climate Centre,China Meteorological Administration,Beijing 100081,China;Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai),Zhuhai 519082,China;Training Centre,China Meteorological Administration,Beijing 100081,China
引用格式:
[1]Qing-Yuan WU;Qing-Quan LI;Yi-Hui DING;Xin-Yong SHEN;Meng-Chu ZHAO;Yu-Xiang ZHU-.Asian summer monsoon responses to the change of land-sea thermodynamic contrast in a warming climate:CMIP6 projections)[J].气候变化研究进展(英文版),2022(02):205-217
A类:
SASM,incon
B类:
Asian,summer,monsoon,responses,land,sea,contrast,warming,climate,CMIP6,projections,It,practical,significance,use,updated,Coupled,Model,Intercomparison,Project,Phase,models,study,impact,changes,under,different,scenarios,compare,similarities,differences,mechanisms,between,regions,this,investigated,future,four,Shared,Socioeconomic,Pathway,using,intensity,South,projected,decrease,by,while,East,EASM,increase,until,21st,century,SSP126,SSP245,SSP370,SSP585,respectively,Moreover,precipitation,remarkably,sistent,trends,Tibetan,Plateau,TP,Northwest,Pacific,tropical,Indian,Ocean,would,greatly,culations,upper,troposphere,surrounding,oceans,greater,than,that,near,surface,smaller,results,weakening,circulation,enhancement,lower,Moisture,budget,analysis,shows,water,vapor,which,thermodynamically,through,anomalous,vertical,moisture,transport,associated,mean,flow,strengthening,meridional,zonal,reduce
AB值:
0.429906
相似文献
Surface air temperature changes over the Tibetan Plateau:Historical evaluation and future projection based on CMIP6 models
Rui Chen;Haoying Li;Xuejia Wang;Xiaohua Gou;Meixue Yang;Guoning Wan-Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research,Potsdam 14473,Germany;Geography Department,Humboldt University of Berlin,Berlin 10099,Germany;IRI THESys,Humboldt University of Berlin,Berlin 10099,Germany;Key Laboratory of Western China's Environmental Systems(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China;Gansu Liancheng Forest Ecosystem Field Observation and Research Station,Lanzhou University,Lanzhou 730333,China;State Key Laboratory of Cryospheric Science,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
Anthropogenic origin of a change in the fire-climate relationship in northern China after~2000 yr BP:Evidence from a 15,500-year black carbon record from Dali Lake
ZHANG Zhiping;LIU Jianbao;CHEN Shengqian;ZHANG Shanjia;JIA Xin;ZHOU Aifeng;ZHAO Jiaju;CHEN Jie;SHEN Zhongwei;CHEN Fahu-Key Laboratory of Western China's Environmental Systems(Ministry of Education),College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China;Group of Alpine Paleoecology and Human Adaptation(ALPHA),State Key Laboratory of Tibetan Plateau Earth System,Resources and Environment(TPESRE),Institute of Tibetan Plateau Research,CAS,Beijing 100101,China;CAS Center for Excellence in Tibetan Plateau Earth Sciences,CAS,Beijing 100101,China;School of Geography,Nanjing Normal University,Nanjing 210023,China;State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,CAS,Xi'an 710061,China
机标中图分类号,由域田数据科技根据网络公开资料自动分析生成,仅供学习研究参考。