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Position and orientation of the westerly jet determined Holocene rainfall patterns in China
Herzschuh, U (Herzschuh, Ulrike)1,2,3; Cao, XY (Cao, Xianyong)1,25; Laepple, T (Laepple, Thomas)1; Dallmeyer, A (Dallmeyer, Anne)4; Telford, RJ (Telford, Richard J.)5,6; Ni, J (Ni, Jian)1,7; Chen, F (Chen, Fahu)8,9; Kong, ZC (Kong, Zhaochen)10; Liu, GX (Liu, Guangxiu)11; Liu, KB (Liu, Kam-Biu)12; Liu, XQ (Liu, Xingqi)13; Stebich, M (Stebich, Martina)14; Tang, LY (Tang, Lingyu)15; Tian, F (Tian, Fang)1; Wang, YB (Wang, Yongbo)1,13; Wischnewski, J (Wischnewski, Juliane)1,16,17; Xu, QH (Xu, Qinghai)18; Yan, S (Yan, Shun)19; Yang, ZJ (Yang, Zhenjing)11,20; Yu, G (Yu, Ge)21; Zhang, Y (Zhang, Yun)10; Zhao, Y (Zhao, Yan)22,23; Zheng, Z (Zheng, Zhuo)24
Source PublicationNATURE COMMUNICATIONS
2019
Volume10Issue:0Pages:2376
DOI10.1038/s41467-019-09866-8
Abstract

Proxy-based reconstructions and modeling of Holocene spatiotemporal precipitation patterns for China and Mongolia have hitherto yielded contradictory results indicating that the basic mechanisms behind the East Asian Summer Monsoon and its interaction with the westerly jet stream remain poorly understood. We present quantitative reconstructions of Holocene precipitation derived from 101 fossil pollen records and analyse them with the help of a minimal empirical model. We show that the westerly jet-stream axis shifted gradually southward and became less tilted since the middle Holocene. This was tracked by the summer monsoon rain band resulting in an early-Holocene precipitation maximum over most of western China, a mid-Holocene maximum in north-central and northeastern China, and a late-Holocene maximum in southeastern China. Our results suggest that a correct simulation of the orientation and position of the westerly jet stream is crucial to the reliable prediction of precipitation patterns in China and Mongolia.

Subject AreaScience & Technology
WOS IDWOS:000469421100013
Language英语
Indexed BySCI
KeywordAsian Summer Monsoon Interannual Variability Precipitation Changes Seasonal Transitions East-asia Climate Model Dataset Circulation Vegetation
WOS Research AreaScience & Technology - Other Topics
WOS SubjectMultidisciplinary Sciences
Cooperation Status国际
ISSN2041-1723
Department高寒生态与人类适应
URL查看原文
PublisherNATURE PUBLISHING GROUP
SubtypeArticle
Citation statistics
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/9296
Collection图书馆
Corresponding AuthorHerzschuh, U (Herzschuh, Ulrike); Cao, XY (Cao, Xianyong)
Affiliation1.Helmholtz Assoc, Alfred Wegener Inst Polar & Marine Res, Polar Terr Environm Syst, D-14473 Potsdam, Germany;
2.Univ Potsdam, Inst Environm Sci & Geog, D-14476 Potsdam, Germany;
3.Univ Potsdam, Inst Biochem & Biol, D-14476 Potsdam, Germany;
4.Max Planck Inst Meteorol, Bundesstr 53, D-20146 Hamburg, Germany;
5.Univ Bergen, Dept Biol Sci, N-5020 Bergen, Norway;
6.Bjerknes Ctr Climate Res, N-5020 Bergen, Norway;
7.Zhejiang Normal Univ, Coll Chem & Life Sci, Jinhua 321004, Zhejiang, Peoples R China;
8.Chinese Acad Sci, Inst Tibetan Plateau Res, CAS Ctr Excellence Tibetan Plateau Earth Sci, Key Lab Alpine Ecol LAE, Beijing 100101, Peoples R China;
9.Lanzhou Univ, Minist Educ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China;
10.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China;
11.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Gansu, Peoples R China;
12.Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA;
13.Capital Normal Univ, Coll Resource Environm & Tourism, Beijing Key Lab Resource Environm & GIS, Beijing 100048, Peoples R China;
14.Senckenberg Res Stn Quaternary Palaeontol, D-99423 Weimar, Germany;
15.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China;
16.Aarhus Univ, Arctic Res Ctr, DK-8000 Aarhus, Denmark;
17.Aarhus Univ, Ctr Environm Humanities, DK-8000 Aarhus, Denmark;
18.Hebei Normal Univ, Coll Resources & Environm Sci, Shijiazhuang 050024, Hebei, Peoples R China;
19.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China;
20.Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazhuang, Hebei, Peoples R China;
21.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;
22.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China;
23.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
24.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangzhou, Guangdong, Peoples R China;
25.Chinese Acad Sci, Inst Tibetan Plateau Res, CAS Ctr Excellence Tibetan Plateau Earth Sci, Key Lab Alpine Ecol LAE, Beijing, Peoples R China.
Recommended Citation
GB/T 7714
Herzschuh, U ,Cao, XY ,Laepple, T ,et al. Position and orientation of the westerly jet determined Holocene rainfall patterns in China[J]. NATURE COMMUNICATIONS,2019,10(0):2376.
APA Herzschuh, U .,Cao, XY .,Laepple, T .,Dallmeyer, A .,Telford, RJ .,...&Zheng, Z .(2019).Position and orientation of the westerly jet determined Holocene rainfall patterns in China.NATURE COMMUNICATIONS,10(0),2376.
MLA Herzschuh, U ,et al."Position and orientation of the westerly jet determined Holocene rainfall patterns in China".NATURE COMMUNICATIONS 10.0(2019):2376.
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