中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Quantitative pollen-based paleoclimate reconstructions for the past 18.5 ka in southwestern Yunnan Province, China

文献类型:期刊论文

作者Xiao, Xiayun1; Zhao, Yan2; Chi, Changting1,3; Zheng, Zhuo4; Ma, Chunmei5; Liang, Chen2; Mao, Limi6; Hillman, Aubrey7
刊名GLOBAL AND PLANETARY CHANGE
出版日期2023-11-01
卷号230页码:19
ISSN号0921-8181
关键词Pollen Quantitative reconstruction Temperature and precipitation Abrupt events Indian summer monsoon Since the last deglaciation Southwestern China
DOI10.1016/j.gloplacha.2023.104288
通讯作者Xiao, Xiayun(xyxiao@niglas.ac.cn)
英文摘要Quantitative reconstruction of past climate plays an important role in understanding global and regional climate changes and validating climate models. Although some important progress has been made in quantitative paleoclimate reconstructions based on terrestrial records in the Indian summer monsoon region, high-resolution quantitative studies spanning the last similar to 20 ka are still relatively sparse with differing results. This study presents high-resolution quantitative variations in mean temperature of the coldest month (MTCM, the first controlling factor of the regional vegetation), mean annual temperature (MAT, the second controlling factor), and mean annual precipitation (MAP) from Lake Tengchongqinghai in southwestern China, based on an updated modern pollen dataset and the fossil pollen record spanning the last 18.5 ka. The results show that temperature and precipitation increased gradually from 18.5 ka, and peaked from 7.2 to 4.5 ka when MAT was on average 1.0 degrees C higher than the modern observational value (14.5 degrees C), corresponding to the mid-Holocene thermal maximum (HTM), and then decreased gradually. The total reconstructed ranges are between-2.2 and 9.2 degrees C for MTCM, 7.7 and 17.2 degrees C for MAT, and 840 and 1300 mm for MAP. On top of this overall climate trend, seven abrupt cold and dry events were detected during the periods of 16.2-14.8 ka, 12.8-11.5 ka, similar to 11.1 ka, 9.1-8.4 ka, similar to 7.7 ka, 4.3-3.7 ka, and 0.68-0.009 ka (1270-1950 CE). The results of this quantitative reconstruction were validated by both statistical and ecological evaluations. We conclude that the trend of climatic change since 18.5 ka in this study area was primarily driven by June, July, August, and September solar insolation and changes in radiative forcing and greenhouse gas concentrations. The abrupt changes may be caused by changes in the Atlantic meridional overturning circulation, solar activity, the position of the Intertropical Convergence Zone, and volcanic activity.
WOS关键词NORTH-ATLANTIC CLIMATE ; INDIAN-SUMMER MONSOON ; ALPINE LACUSTRINE RECORD ; EASTERN TIBETAN PLATEAU ; LAST GLACIAL MAXIMUM ; GREENLAND ICE CORE ; ASIAN MONSOON ; HIGH-RESOLUTION ; CALIBRATION-SET ; ABRUPT CHANGES
资助项目National Key Research and Development Program of China[2016YFA0600501] ; National Natural Science Foundation of China[41877434] ; National Natural Science Foundation of China[42077424] ; National Natural Science Foundation of China[42277446] ; National Natural Science Foundation of China[41877437]
WOS研究方向Physical Geography ; Geology
语种英语
出版者ELSEVIER
WOS记录号WOS:001110732600001
资助机构National Key Research and Development Program of China ; National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/202559]  
专题中国科学院地理科学与资源研究所
通讯作者Xiao, Xiayun
作者单位1.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Prov Key Lab Geodynam & Geohazards, Guangzhou 510275, Peoples R China
5.Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Peoples R China
6.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
7.SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA
推荐引用方式
GB/T 7714
Xiao, Xiayun,Zhao, Yan,Chi, Changting,et al. Quantitative pollen-based paleoclimate reconstructions for the past 18.5 ka in southwestern Yunnan Province, China[J]. GLOBAL AND PLANETARY CHANGE,2023,230:19.
APA Xiao, Xiayun.,Zhao, Yan.,Chi, Changting.,Zheng, Zhuo.,Ma, Chunmei.,...&Hillman, Aubrey.(2023).Quantitative pollen-based paleoclimate reconstructions for the past 18.5 ka in southwestern Yunnan Province, China.GLOBAL AND PLANETARY CHANGE,230,19.
MLA Xiao, Xiayun,et al."Quantitative pollen-based paleoclimate reconstructions for the past 18.5 ka in southwestern Yunnan Province, China".GLOBAL AND PLANETARY CHANGE 230(2023):19.

入库方式: OAI收割

来源:地理科学与资源研究所

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