Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1186/s40645-016-0080-y |
Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau | |
Tada, Ryuji1; Zheng, Hongbo2; Clift, Peter D.3 | |
通讯作者 | Tada, Ryuji |
来源期刊 | PROGRESS IN EARTH AND PLANETARY SCIENCE
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ISSN | 2197-4284 |
出版年 | 2016 |
卷号 | 3 |
英文摘要 | Uplift of the Himalaya and Tibetan Plateau (HTP) and its linkage with the evolution of the Asian monsoon has been regarded as a typical example of a tectonic-climate linkage. Although this linkage remains unproven because of insufficient data, our understanding has greatly advanced in the past decade. It is thus timely to summarize our knowledge of the uplift history of the HTP, the results of relevant climate simulations, and spatiotemporal changes in the Indian and East Asian monsoons since the late Eocene. Three major pulses of the HTP uplift have become evident: (1) uplift of the southern and central Tibetan Plateau (TP) at ca. 40-35 Ma, (2) uplift of the northern TP at ca. 25-20 Ma, and (3) uplift of the northeastern to eastern TP at ca. 15-10 Ma. Modeling predictions suggest that (i) uplift of the southern and central TP should have intensified the Indian summer monsoon (ISM) and the Somali Jet at 40-35 Ma; (ii) uplift of the northern TP should have intensified the East Asian summer monsoon (EASM) and East Asian winter monsoon (EAWM), as well as the desertification of inland Asia at 25-20 Ma; and (iii) uplift of the northeastern and eastern TP should have further intensified the EASM and EAWM at 15-10 Ma. We tested these predictions by comparing them with paleoclimate data for the time intervals of interest. There are insufficient paleoclimate data to test whether the ISM and Somali Jet intensified with the uplift of the southern and central TP at 40-35 Ma, but it is possible that such uplift enhanced erosion and weathering that drew down atmospheric CO2 and resulted in global cooling. There is good evidence that the EASM and EAWM intensified, and desertification started in inland Asia at 25-20 Ma in association with the uplift of the northern TP. The impact of the uplift of the northeastern and eastern TP on the Asian monsoon at 15-10 Ma is difficult to evaluate because that interval was also a time of global cooling and Antarctic glaciation that might also have influenced the intensity of the Asian monsoon. |
英文关键词 | East Asian summer monsoon East Asian winter monsoon Indian summer monsoon Himalaya Tibetan Plateau Chinese Loess Plateau Climate model Tectonic-climate linkage Westerly jet Desertification |
类型 | Review |
语种 | 英语 |
国家 | Japan ; Peoples R China ; USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000381923000001 |
WOS关键词 | CHINESE LOESS PLATEAU ; LATE CENOZOIC UPLIFT ; APATITE FISSION-TRACK ; LARGE-SCALE OROGRAPHY ; LATE MIOCENE ; SUMMER MONSOON ; WINTER MONSOON ; CLIMATE-CHANGE ; XINING BASIN ; LATE EOCENE |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/195758 |
作者单位 | 1.Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Bunkyo Ku, 7-3-1 Hongo, Tokyo 1130033, Japan; 2.Nanjing Normal Univ, Sch Geog Sci, 1 Wenyuan Rd, Nanjing, Jiangsu, Peoples R China; 3.Louisiana State Univ, Dept Geol & Geophys, E235 Howe Russell Kniffen Geosci Complex, Baton Rouge, LA 70803 USA |
推荐引用方式 GB/T 7714 | Tada, Ryuji,Zheng, Hongbo,Clift, Peter D.. Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau[J],2016,3. |
APA | Tada, Ryuji,Zheng, Hongbo,&Clift, Peter D..(2016).Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau.PROGRESS IN EARTH AND PLANETARY SCIENCE,3. |
MLA | Tada, Ryuji,et al."Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau".PROGRESS IN EARTH AND PLANETARY SCIENCE 3(2016). |
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