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
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出版日期 | 2021-03-23 |
卷号 | 12期号:1页码:9 |
ISSN号 | 2041-1723 |
DOI | 10.1038/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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