中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Northwestward Migration of the Northern Edge of the East Asian Summer Monsoon During the Mid-Pliocene Warm Period: Simulations and Reconstructions

文献类型:期刊论文

作者Huang, Xiaofang1,2,3; Jiang, Dabang3,4,5; Dong, Xinxin6; Yang, Shiling1,2,3; Su, Baohuang4; Li, Xiangyu4; Tang, Zihua1,2; Wang, Yongda1,2,3
刊名JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
出版日期2019-02-16
卷号124期号:3页码:1392-1404
关键词mid-Pliocene PlioMIP northern edge of the East Asian summer monsoon western Pacific subtropical high
ISSN号2169-897X
DOI10.1029/2018JD028995
英文摘要The mid-Pliocene (similar to 3.3-3.0Ma) was the most recent warm interval during which atmospheric CO2 concentrations were similar to the present level of similar to 400ppmv. Therefore, it is often regarded as an analog for a near-future climate scenario. To examine the behavior of the East Asian summer monsoon (EASM) during the mid-Pliocene warm period, the northern edge of the EASM, a sensitive indicator of the advance and retreat of the summer monsoon rainbelt, was analyzed using the output of the Pliocene Model Intercomparison Project Phase 1. The results show a similar to 150-km-northwestward migration of the northern edge of the EASM during the mid-Pliocene compared to the preindustrial period, which is consistent with that derived from a comparison of geological records and modern observations. However, the geological records indicate a greater east-west climatic contrast during the Pliocene than at present, which requires investigation in future modeling studies. The simulations also show a substantial increase in the large-scale land-sea thermal contrast between the East Asian mainland and the equatorial western Pacific during the interval of mid-Pliocene warmth. This led to the intensification and westward extension of the western Pacific subtropical high, causing a northwestward shift of the EASM and the resulting mitigation of drought in northern China. We suggest that global warming will shift the EASM northwestward mainly via changes in the position and intensity of the western Pacific subtropical high; this requires systematic studies in the future based on meteorological observations and simulations.
WOS关键词CHINESE LOESS PLATEAU ; RED CLAY FORMATION ; PLIOMIP EXPERIMENTAL-DESIGN ; LATE MIOCENE ; POLLEN RECORD ; VEGETATION EVOLUTION ; CLIMATE VARIABILITY ; ICE-SHEET ; MODEL ; PLEISTOCENE
资助项目National Natural Science Foundation of China[41725010] ; National Natural Science Foundation of China[41672175] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19050104] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000459377000014
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/90692]  
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Yang, Shiling
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
2.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
4.Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
5.Chengdu Univ Informat Technol, Joint Lab Climate & Environm Change, Chengdu, Sichuan, Peoples R China
6.Chinese Acad Sci, Bur Gen Affairs, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Huang, Xiaofang,Jiang, Dabang,Dong, Xinxin,et al. Northwestward Migration of the Northern Edge of the East Asian Summer Monsoon During the Mid-Pliocene Warm Period: Simulations and Reconstructions[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(3):1392-1404.
APA Huang, Xiaofang.,Jiang, Dabang.,Dong, Xinxin.,Yang, Shiling.,Su, Baohuang.,...&Wang, Yongda.(2019).Northwestward Migration of the Northern Edge of the East Asian Summer Monsoon During the Mid-Pliocene Warm Period: Simulations and Reconstructions.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(3),1392-1404.
MLA Huang, Xiaofang,et al."Northwestward Migration of the Northern Edge of the East Asian Summer Monsoon During the Mid-Pliocene Warm Period: Simulations and Reconstructions".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.3(2019):1392-1404.

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来源:地质与地球物理研究所

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