中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene

文献类型:期刊论文

作者Cheng, Jun1,6; Wu, Haibin2,3; Liu, Zhengyu9; Gu, Peng6; Wang, Jingjing8; Zhao, Cheng7,8; Li, Qin1; Chen, Haishan6; Lu, Huayu8; Hu, Haibo4
刊名NATURE COMMUNICATIONS
出版日期2021-03-23
卷号12期号:1页码:9
ISSN号2041-1723
DOI10.1038/s41467-021-22087-2
英文摘要One long-standing issue in the paleoclimate records is whether East Asian Summer Monsoon peaked in the early Holocene or mid-Holocene. Here, combining a set of transient earth system model simulations with proxy records, we propose that, over northern China, monsoon rainfall peaked in the early Holocene, while soil moisture and tree cover peaked in the mid-Holocene. The delayed ecosystem (soil moisture and tree cover) response to rainfall is caused by the vegetation response to winter warming and the subsequent feedback with soil moisture. Our study provides a mechanism for reconciling different evolution behaviors of monsoon proxy records; it sheds light on the driving mechanism of the monsoon evolution and monsoon-ecosystem feedback over northern China, with implications to climate changes in other high climate sensitivity regions over the globe. How the East Asian Summer Monsoon has changed over the Holocene has been debated, as some proxy records disagree with each other. Here, the authors suggest that monsoonal rainfall peaked in the early Holocene, while ecosystem responses peaked in the mid-Holocene, explaining the differences between records.
WOS关键词NORTHERN CHINA ; CLIMATE ; MODEL ; TEMPERATURE ; SURFACE ; RECONSTRUCTION ; PRECIPITATION ; DEGLACIATION ; SIMULATION ; EVOLUTION
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA13010106] ; NSFC[41888101] ; MOST[2017YFA0603801] ; US NSF P2C2 ; [MOST2016YFA0600504] ; [NSFC41630527]
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000684714900003
出版者NATURE PORTFOLIO
资助机构Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; NSFC ; NSFC ; NSFC ; NSFC ; MOST ; MOST ; MOST ; MOST ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; NSFC ; NSFC ; NSFC ; NSFC ; MOST ; MOST ; MOST ; MOST ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; NSFC ; NSFC ; NSFC ; NSFC ; MOST ; MOST ; MOST ; MOST ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; NSFC ; NSFC ; NSFC ; NSFC ; MOST ; MOST ; MOST ; MOST ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2 ; US NSF P2C2
源URL[http://ir.iggcas.ac.cn/handle/132A11/101887]  
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Cheng, Jun; Wu, Haibin; Liu, Zhengyu
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
4.Nanjing Univ, Sch Atmospher Sci, Nanjing, Peoples R China
5.Peking Univ, Dept Atmospher & Ocean Sci Sch Phys, Lab Climate & Ocean Atmosphere Studies LaCOAS, Beijing, Peoples R China
6.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Joint Int Res Lab Climate & Environm Change ILCE, Key Lab Meteorol Disaster,Minist Educ KLME, Nanjing, Peoples R China
7.CAS Ctr Excellence Quaternary Sci & Global Change, Xian, Peoples R China
8.Nanjing Univ, Sch Geog & Ocean Sci, Nanjing, Peoples R China
9.Ohio State Univ, Dept Geog, Atmospher Sci Program, Columbus, OH 43210 USA
推荐引用方式
GB/T 7714
Cheng, Jun,Wu, Haibin,Liu, Zhengyu,et al. Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene[J]. NATURE COMMUNICATIONS,2021,12(1):9.
APA Cheng, Jun.,Wu, Haibin.,Liu, Zhengyu.,Gu, Peng.,Wang, Jingjing.,...&Song, Yaoming.(2021).Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene.NATURE COMMUNICATIONS,12(1),9.
MLA Cheng, Jun,et al."Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene".NATURE COMMUNICATIONS 12.1(2021):9.

入库方式: OAI收割

来源:地质与地球物理研究所

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