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  4. 中国科学院新生代地质与环境重点实验室
Impact of the uplift of the Central Asian Orogenic Belt and NE Tibetan Plateau on the East Asian climate since the late Miocene

文献类型：期刊论文

作者Zhang, Ran2,3; Jiang, Dabang2; Zhang, Jian1,7; Zhang, Chunxia6; Yang, Yibo5; Jia, Yunxia4; Wang, Na2
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2023-04-01
卷号615页码:10
关键词Late Miocene East Asia Central Asian Orogenic Belt NE Tibetan Plateau
ISSN号0031-0182
DOI10.1016/j.palaeo.2023.111451
英文摘要The uplift of the Central Asian Orogenic Belt (CAOB) and the northeastern (NE) Tibetan Plateau has exerted an important effect on the evolution of the East Asian climate since the late Miocene. However, previous modeling studies were generally based on modern boundary conditions, a direct comparison between the impacts of the uplift of the CAOB and NE Tibetan Plateau was still absent, and the climatic effects of the uplift of these mountains since the late Miocene remain ambiguous. Here, we use the Community Atmosphere Model version 4 (CAM4) with a high horizontal resolution (similar to 0.63 degrees x 0.47 degrees) combined with late Miocene boundary conditions to investigate the effects of the CAOB and NE Tibetan Plateau uplift on the East Asian climate since the late Miocene. The results indicate that the combined uplift of these landmasses increased the annual precipitation in the uplifted regions and eastern Asia, decreased the annual precipitation in central Asia, strengthened summer monsoon winds over northern East Asia, weakened winter monsoon winds over southern East Asia, and strengthened summer and winter high tropospheric westerly wind at northern high latitudes. Of the two uplifting landmasses, the uplift of the CAOB increased the summer precipitation and strengthened the summer high tropospheric westerly wind at higher latitudes and had a greater impact on the changes in winter monsoon winds and winter high tropospheric westerly wind. By comparison, the uplift of the NE Tibetan Plateau was also important in some aspects, such as the increased annual precipitation in eastern Asia. These results emphasized the important climate effects of the CAOB and NE Tibetan Plateau on the East Asian climate and improved our understanding of the dynamic link between orogenic evolution and paleoclimatic change since the late Miocene.
WOS关键词STEPWISE ARIDIFICATION ; MONSOON PRECIPITATION ; ISOTOPIC EVIDENCE ; MA ; RECORD ; MAGNETOSTRATIGRAPHY ; INTENSIFICATION ; VEGETATION ; EVOLUTION ; TIANSHAN
资助项目National Natural Science Founda-tion of China[41888101] ; Second Tibetan Plateau Scientific Expedition and Research Program[2019QZKK0101] ; National NaturalScience Foundation of China[42071113]
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
WOS记录号WOS:000993762000001
出版者ELSEVIER
资助机构National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National NaturalScience Foundation of China ; National NaturalScience Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National NaturalScience Foundation of China ; National NaturalScience Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National NaturalScience Foundation of China ; National NaturalScience Foundation of China ; National Natural Science Founda-tion of China ; National Natural Science Founda-tion of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; National NaturalScience Foundation of China ; National NaturalScience Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110954]  
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Zhang, Ran
作者单位1.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteorol, Nanjing 210044, Peoples R China
2.Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Inst Atmospher Phys, POB 9804, Beijing 100029, Peoples R China
4.Shanxi Normal Univ, Sch Geog Sci, Taiyuan 030031, Peoples R China
5.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Sci Resou, Beijing 100101, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
7.Peking Univ, Sch Phys, Dept Atmosphere & Ocean Sci, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714		 Zhang, Ran,Jiang, Dabang,Zhang, Jian,et al. Impact of the uplift of the Central Asian Orogenic Belt and NE Tibetan Plateau on the East Asian climate since the late Miocene[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2023,615:10.
APA Zhang, Ran.,Jiang, Dabang.,Zhang, Jian.,Zhang, Chunxia.,Yang, Yibo.,...&Wang, Na.(2023).Impact of the uplift of the Central Asian Orogenic Belt and NE Tibetan Plateau on the East Asian climate since the late Miocene.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,615,10.
MLA Zhang, Ran,et al."Impact of the uplift of the Central Asian Orogenic Belt and NE Tibetan Plateau on the East Asian climate since the late Miocene".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 615(2023):10.

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来源：地质与地球物理研究所

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