TitleMultispherical interactions and their effects on the Tibetan Plateau's earth system: a review of the recent researches
AuthorsYao, Tandong
Wu, Fuyuan
Ding, Lin
Sun, Jimin
Zhu, Liping
Piao, Shilong
Deng, Tao
Ni, Xijun
Zheng, Hongbo
Ouyang, Hua
AffiliationChinese Acad Sci, Ctr Excellence Tibetan Earth Sci, Beijing 100101, Peoples R China.
Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China.
Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China.
Peking Univ, Dept Ecol, Coll Urban & Environm Sci, Beijing 100871, Peoples R China.
Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China.
Nanjing Normal Univ, Sch Geog Sci, Nanjing 210023, Jiangsu, Peoples R China.
Chinese Acad Sci, Inst Geog Sci & Nat Resources, Beijing 100101, Peoples R China.
Chinese Acad Sci, Cold & Arid Environm & Engn Inst, Lanzhou 730000, Peoples R China.
KeywordsTibetan Plateau
multispherical interactions
effects
SOUTHERN TIBET
LUNPOLA BASIN
PALEO-ALTIMETRY
VOLCANIC-ROCKS
AMERICAN-WEST
LAST DECADE
UPLIFT
GANGDESE
CLIMATE
EVOLUTION
Issue Date2015
PublisherNATIONAL SCIENCE REVIEW
CitationNATIONAL SCIENCE REVIEW.2015,2,(4),468-488.
AbstractThe 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.
URIhttp://hdl.handle.net/20.500.11897/439135
ISSN2095-5138
DOI10.1093/nsr/nwv070
IndexedSCI(E)
Appears in Collections:城市与环境学院

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