IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2010~)
A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon
Zhang, Haiwei1,2; Zhang, Xu3,4,5; Cai, Yanjun1,2; Sinha, Ashish6; Spoetl, Christoph7; Baker, Jonathan1; Kathayat, Gayatri1; Liu, Zhengyu8; Tian, Ye1; Lu, Jiayu1; Wang, Zhenqian3; Zhao, Jingyao1; Jia, Xuexue1; Du, Wenjing1; Ning, Youfeng1; An, Zhisheng2; Edwards, R. Lawrence9; Cheng, Hai1,2,10
Corresponding AuthorZhang, Haiwei(zhanghaiwei@xjtu.edu.cn) ; Cheng, Hai(cheng021@xjtu.edu.cn)
2021-06-01
Source PublicationQUATERNARY SCIENCE REVIEWS
ISSN0277-3791
Volume261Pages:18
AbstractConflicting reconstructions of Holocene variability of the East Asian summer monsoon (EASM) from speleothem versus other types of proxy records have yielded widely divergent estimates of its phase relationship with the Indian summer monsoon (ISM) and Northern Hemisphere summer insolation (NHSI). This apparent discrepancy has been partly attributed to the uncertainties in the climatic representation of Chinese speleothem oxygen isotope (delta O-18) records. Here we present a composite speleothem delta O-18 record of the last similar to 14 kyr from Shennong Cave in southeastern China and model-simulated data of rainfall and meteoric delta O-18 over eastern China. Our synthesis of the proxy-model data suggests that the spatial patterns in both speleothem delta O-18 and paleo-rainfall over eastern China during the Holocene are diverse at orbital and multi-millennial scales. Our findings imply that: 1) speleothem delta O-18 in the EASM regime is largely controlled by the large-scale circulation and concomitant latitudinal shifts of the monsoon rain belt; notwithstanding the heterogeneous spatiotemporal pattern of Holocene rainfall as inferred from various proxy records, a coherent orbital-scale speleothem delta O-18 variability across most Asian monsoon regions (except southeastern China) indeed stems from the NHSI-forced changes in overall monsoon intensity; overall monsoon intensity is not equivalent to monsoon rainfall amount but a manifestation of the large-scale atmospheric circulation; 2) divergent phase relationships with NHSI between speleothem delta O-18 and other proxy records are consistent withdrather than contradictory todthe NHSI forcing mechanism. Speleothem delta O-18 and rainfall records reflect two different aspects of the monsoon dynamics. These results may thus, largely help to reconcile the divergent views of the Holocene Asian monsoon variability. (C) 2021 Elsevier Ltd. All rights reserved.
KeywordSpeleothem East Asian summer monsoon (EASM) Holocene Spatiotemporal pattern Northern hemisphere summer insolation (NHSI)
DOI10.1016/j.quascirev.2021.106911
WOS KeywordCHINESE CAVE RECORDS ; HIGH-RESOLUTION ; SOUTHEASTERN CHINA ; STALAGMITE RECORD ; CLIMATE CHANGES ; OXYGEN-ISOTOPE ; PRECIPITATION SEASONALITY ; FORCING MECHANISMS ; DELTA-O-18 RECORD ; SOUTHERN CHINA
Indexed BySCI ; SCI
Language英语
Funding ProjectNational Science Foundation of China[41888101] ; National Science Foundation of China[41972186] ; National Key Research and Development Program of China[2017YFA0603401] ; China Postdoctoral Science Foundation[2019T120894]
WOS Research AreaPhysical Geography ; Geology
Funding OrganizationNational Science Foundation of China ; National Key Research and Development Program of China ; China Postdoctoral Science Foundation
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary
WOS IDWOS:000653082100009
PublisherPERGAMON-ELSEVIER SCIENCE LTD
Citation statistics
Cited Times:12[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/16739
Collection黄土与第四纪地质国家重点实验室(2010~)
第四纪科学与全球变化卓越创新中心
Corresponding AuthorZhang, Haiwei; Cheng, Hai
Affiliation1.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710054, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
3.Lanzhou Univ, Coll Earth & Environm Sci, Ctr Pan Pole Environm Pan TPE 3, Key Lab Western Chinas Environm Syst,Minist Educ, Lanzhou 730000, Peoples R China
4.Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bussestr 24, D-27570 Bremerhaven, Germany
5.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
6.Calif State Univ Dominguez Hills, Dept Earth Sci, Carson, CA 90747 USA
7.Univ Innsbruck, Inst Geol, A-6020 Innsbruck, Austria
8.Ohio State Univ, Dept Geog, Columbus, OH 43210 USA
9.Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
10.CAGS, Key Lab Karst Dynam, MLR, Inst Karst Geol, Guilin, Peoples R China
Recommended Citation
GB/T 7714
Zhang, Haiwei,Zhang, Xu,Cai, Yanjun,et al. A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon[J]. QUATERNARY SCIENCE REVIEWS,2021,261:18.
APA Zhang, Haiwei.,Zhang, Xu.,Cai, Yanjun.,Sinha, Ashish.,Spoetl, Christoph.,...&Cheng, Hai.(2021).A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon.QUATERNARY SCIENCE REVIEWS,261,18.
MLA Zhang, Haiwei,et al."A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon".QUATERNARY SCIENCE REVIEWS 261(2021):18.
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