Multispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches

被引:29
作者
Tandong Yao [1 ,2 ,3 ]
Fuyuan Wu [1 ,4 ]
Lin Ding [1 ,2 ]
Jimin Sun [1 ,4 ]
Liping Zhu [1 ,2 ]
Shilong Piao [1 ,2 ,5 ]
Tao Deng [1 ,6 ]
Xijun Ni [1 ,6 ]
Hongbo Zheng [1 ,7 ]
Hua Ouyang [8 ]
机构
[1] Center for Excellence in Tibetan Earth Sciences, Chinese Academy of Sciences
[2] Institute of Tibetan Plateau Research,Chinese Academy of Sciences
[3] Cold and Arid Environment and Engineering Institute, Chinese Academy of Sciences
[4] Institute of Geology and Geophysics,Chinese Academy of Sciences
[5] Department of Ecology, College of Urban and Environmental Sciences, Peking University
[6] Key Laboratory of Vertebrate Evolution and Human Origins,Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Sciences
[7] School ofGeographical Sciences, Nanjing Normal University
[8] Institute of Geographical Sciences and Natural Resources, Chinese Academy of Sciences
关键词
Tibetan Plateau; multispherical interactions; efects;
D O I
暂无
中图分类号
P31 [大地(岩石界)物理学(固体地球物理学)]; P53 [历史地质学、地层学];
学科分类号
070801 ; 070903 ;
摘要
The Tibetan Plateau(TP) is a regional Earth system showing very strong interactions among its lithosphere, hydrosphere, cryosphere, biosphere, atmosphere, and anthrosphere. hese interactions manifest TP’s impact on surrounding regions and relect 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 heir Resource-Environment Signiicance(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, uplit 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 ield investigations have been conducted to obtain data about stratum, paleontology, paleoenvironment, genetic diferentiation of animals and plants. We have developed conceptual and mathematical models for crust uplit formation, paleoclimate, glacial melt,water–air interface lux, 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 uplit 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. he scientiic results can play fundamental roles in supporting the TP’s resource exploration and societal sustainable development.
引用
收藏
页码:468 / 488
页数:21
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