Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau
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- 作者：Ryuji Tada ; Hongbo Zheng ; Peter D. Clift
- 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
- 刊名：Progress in Earth and Planetary Science
- 出版年：2016
- 出版时间：December 2016
- 年：2016
- 卷：3
- 期：1
- 全文大小：3,607 KB
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Hongbo Zheng (2)
Peter D. Clift (3)
1. Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan
2. School of Geography Science, Nanjing Normal University, 1 Wenyuan Road, Xianlin University Town, Nanjing, China
3. Department of Geology and Geophysics, E235 Howe-Russell-Kniffen Geoscience Complex, Louisiana State University, Baton Rouge, LA, 70803, USA - 刊物类别：Earth Sciences, general; Geophysics/Geodesy; Planetology; Biogeosciences; Hydrogeology; Atmospheric
- 刊物主题：Earth Sciences, general; Geophysics/Geodesy; Planetology; Biogeosciences; Hydrogeology; Atmospheric Sciences;
- 出版者：Springer Berlin Heidelberg
- ISSN：2197-4284
文摘
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. Keywords 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