中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data-model comparison

文献类型:期刊论文

作者Sun, Yong2,9,10; Wu, Haibin3,4,5; Ramstein, Gilles2; Liu, Bo6; Zhao, Yan9; Li, Laurent1; Yuan, Xiayu7; Zhang, Wenchao3; Li, Lijuan10; Zou, Liwei10
刊名CLIMATE DYNAMICS
出版日期2022-06-17
页码14
ISSN号0930-7575
关键词Mid-Holocene Monsoon precipitation Data-model comparison Water vapor budget Thermodynamic effect Dynamic effect Cloud cooling effect
DOI10.1007/s00382-022-06359-1
英文摘要The mid-Holocene (MH; 6 ka) is one of the benchmark periods for the Paleoclimate Modeling Intercomparison Project (PMIP) and provides a unique opportunity to study monsoon dynamics and orbital forcing (i.e., mostly precession) that differ significantly from the present day. We conducted a data-model comparison along with a dynamic analysis to investigate monsoonal (i.e., East Asian summer monsoon; EASM) precipitation changes over East Asia during the MH. We used the three phases of the PMIP simulations for the MH, and quantitatively compare model results with pollen-based climate records. The data-model comparison shows an overall increase in the summer monsoon precipitation, except a local decrease during the MH. Decomposition of the moisture budget into thermodynamic and dynamic components allows us to assess their relative role in controlling EASM precipitation during the MH, and to investigate the precipitation changes obtained from pollen records in terms of physical processes. We show that the dynamic effect, rather than the thermodynamic effect, is the dominant control in increased EASM precipitation during the MH in both the proxy records and models. The dynamic increase in precipitation results mainly from the enhancement of horizontal monsoonal moisture transport that is caused by intensified stationary eddy horizontal circulation over East Asia. In addition, a cloud-related cooling effect reduced the thermodynamic contribution to the increase in EASM precipitation during the MH.
WOS关键词INDIVIDUAL FEEDBACK PROCESSES ; LAST GLACIAL MAXIMUM ; CLIMATIC CHANGES ; AFRICAN MONSOON ; GREEN SAHARA ; POLLEN DATA ; PALEOCLIMATE ; SIMULATIONS ; FRAMEWORK
资助项目National Key Research and Development Program of China[2018YFA0606003] ; National Program on Key Basic Research Project of China[2017YFA0604601] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program[2019QZKK0102] ; NSFC[41505076] ; NSFC[41572165]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者SPRINGER
WOS记录号WOS:000812488400004
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Program on Key Basic Research Project of China ; National Program on Key Basic Research Project of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; NSFC ; NSFC ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Program on Key Basic Research Project of China ; National Program on Key Basic Research Project of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; NSFC ; NSFC ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Program on Key Basic Research Project of China ; National Program on Key Basic Research Project of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; NSFC ; NSFC ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Program on Key Basic Research Project of China ; National Program on Key Basic Research Project of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; NSFC ; NSFC
源URL[http://ir.iggcas.ac.cn/handle/132A11/106077]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Sun, Yong
作者单位1.Sorbonne Univ, CNRS, Lab Meteorol Dynam, Ecole Polytech,Ecole Normale Super, Paris, France
2.Univ Paris Saclay, Lab Sci Climat & Environnem, LSCE IPSL, CEA CNRS UVSQ, Gif Sur Yvette, France
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
4.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.China Univ Geosci, Sch Environm Studies, Dept Atmospher Sci, Wuhan 430074, Peoples R China
7.Chinese Acad Sci, Inst Atmospher Phys, Editorial Off Adv Atmospher Sci, Beijing 100029, Peoples R China
8.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
9.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst, Resources & Environm TPESRE, Beijing 100101, Peoples R China
10.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Sun, Yong,Wu, Haibin,Ramstein, Gilles,et al. Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data-model comparison[J]. CLIMATE DYNAMICS,2022:14.
APA Sun, Yong.,Wu, Haibin.,Ramstein, Gilles.,Liu, Bo.,Zhao, Yan.,...&Zhou, Tianjun.(2022).Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data-model comparison.CLIMATE DYNAMICS,14.
MLA Sun, Yong,et al."Revisiting the physical mechanisms of East Asian summer monsoon precipitation changes during the mid-Holocene: a data-model comparison".CLIMATE DYNAMICS (2022):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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