Climate Change Data Portal
DOI | 10.1038/s41467-021-22087-2 |
Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene | |
Cheng J.; Wu H.; Liu Z.; Gu P.; Wang J.; Zhao C.; Li Q.; Chen H.; Lu H.; Hu H.; Gao Y.; Yu M.; Song Y. | |
发表日期 | 2021 |
ISSN | 2041-1723 |
卷号 | 12期号:1 |
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. © 2021, The Author(s). |
语种 | 英语 |
scopus关键词 | climate change; climate modeling; ecosystem response; Holocene; monsoon; paleoclimate; proxy climate record; rainfall; soil moisture; soil-vegetation interaction; summer; China |
来源期刊 | Nature Communications |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/250733 |
作者单位 | Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, China; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China; CAS Center for Excellence in Life and Paleoenvironment, Beijing, China; University of Chinese Academy of Sciences, Beijing, China; Atmospheric Science Program, Department of Geography, The Ohio State University, Columbus, OH, United States; School of Geography and Ocean Science, Nanjing University, Nanjing, China; CAS Center for Excellence in Quaternary Science and Global Change, Xian, China; School of Atmospheric Sciences, Nanjing University, Nanjing, China; Laboratory for Climate and Ocean-Atmosphere Studies (LaCOAS) and Department of Atmospheric and ... |
推荐引用方式 GB/T 7714 | Cheng J.,Wu H.,Liu Z.,et al. Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene[J],2021,12(1). |
APA | Cheng J..,Wu H..,Liu Z..,Gu P..,Wang J..,...&Song Y..(2021).Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene.Nature Communications,12(1). |
MLA | Cheng J.,et al."Vegetation feedback causes delayed ecosystem response to East Asian Summer Monsoon Rainfall during the Holocene".Nature Communications 12.1(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Cheng J.]的文章 |
[Wu H.]的文章 |
[Liu Z.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Cheng J.]的文章 |
[Wu H.]的文章 |
[Liu Z.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Cheng J.]的文章 |
[Wu H.]的文章 |
[Liu Z.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。