Multispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches
文献类型:期刊论文
作者 | Yao T.; Wu, F.; Ding, L.; Sun, J.; Zhu, L.; Piao, S. L.; Deng, T.; Ni, X.; Zheng, H.; Ouyang, H. |
刊名 | National Science Review
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出版日期 | 2015 |
卷号 | 2期号:4页码:468-488 |
关键词 | Tibetan Plateau multispherical interactions effects southern tibet lunpola basin paleo-altimetry volcanic-rocks american-west last decade uplift gangdese climate evolution |
ISSN号 | 2095-5138 |
DOI | 10.1093/nsr/nwv070 |
英文摘要 | The Tibetan Plateau (TP) is a regional Earth system showing very strong interactions among its lithosphere, hydrosphere, cryosphere, biosphere, atmosphere, and anthrosphere. These interactions manifest TP's impact on surrounding regions and reflect TP's response to the global change. Quantifying the multispherical interactions is critically important to understand the TP environment. Our recent years researches including the ongoing program entitled 'Tibetan Multi-Spheres Interactions and Their Resource-Environment Significance (TIMI)', the completed program entitled. 'Paleo-Altitudes of Tibetan Plateau and Environment (PATE)', as well as the other relating projects have focused on multidisciplinary research approaches and emphasized on three major pathways: Eurasia-Indian plates collision on deep-Earth dynamics, uplift impact on Earth's mantle crust dynamics, and contemporary interface on land surface and atmospheric dynamics. Our researches have taken in situ measurement as priority and developed several platforms of data acquisition and analysis, including the platforms of water-phase transformations, and ecosystem observations. Our field investigations have been conducted to obtain data about stratum, paleontology, paleoenvironment, genetic differentiation of animals and plants. We have developed conceptual and mathematical models for crust uplift formation, paleoclimate, glacial melt, water air interface flux, vegetation climate, and soil erosion. We have also assessed the anthropogenic impacts on environment. Our researches have achieved new and reliable redating of the mantle crust interaction and initial formation of the TP, found the interaction between tectonics and uplift of the TP and resultant paleoaltitude acting as a spreading source; discovered the interaction between the westerlies and Indian monsoon acting as a control chain that dominates the TP's contemporary environment. The scientific results can play fundamental roles in supporting the TP's resource exploration and societal sustainable development. |
语种 | 英语 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/43591] ![]() |
专题 | 地理科学与资源研究所_历年回溯文献 |
推荐引用方式 GB/T 7714 | Yao T.,Wu, F.,Ding, L.,et al. Multispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches[J]. National Science Review,2015,2(4):468-488. |
APA | Yao T..,Wu, F..,Ding, L..,Sun, J..,Zhu, L..,...&Ouyang, H..(2015).Multispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches.National Science Review,2(4),468-488. |
MLA | Yao T.,et al."Multispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches".National Science Review 2.4(2015):468-488. |
入库方式: OAI收割
来源:地理科学与资源研究所
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