Land–atmosphere–ocean coupling associated with the Tibetan Plateau and its climate impacts

被引：27

作者：

Yimin Liu ^{[1
,2
,3
]}

Mengmeng Lu ^{[4
,5
]}

Haijun Yang ^{[6
]}

Anmin Duan ^{[1
,2
,3
]}

Bian He ^{[1
,2
,3
]}

Song Yang ^{[4
,7
]}

Guoxiong Wu ^{[1
,2
]}

机构：

[1] State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics,Chinese Academy of Sciences (CAS)

[2] College of Earth Science, University of Chinese Academy of Sciences

[3] CAS Center for Excellence in Tibetan Plateau Earth Sciences

[4] School of Atmospheric Sciences& Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University

[5] Department of Earth and Planetary Sciences, Harvard University

[6] Laboratory for Climate and Ocean-Atmosphere Studies (LaCOAS) and Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University

[7] Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)

来源：

National Science Review | 2020年 / 7卷 / 03期

关键词：

Tibetan and Iranian Plateau system; atmospheric heat source; Asian summer monsoon; upstream climate; Atlantic Meridional Overturning Circulation;

D O I：

暂无

中图分类号：

P461 [气候的形成和影响气候的因素]; P732 [海洋气象学];

学科分类号：

0706 ; 070601 ;

摘要：

This paper reviews recent advances regarding land–atmosphere–ocean coupling associated with the Tibetan Plateau(TP) and its climatic impacts. Thermal forcing over the TP interacts strongly with that over the Iranian Plateau, forming a coupled heating system that elevates the tropopause, generates a monsoonal meridional circulation over South Asia and creates conditions of large-scale ascent favorable for Asian summer monsoon development. TP heating leads to intensification and westward extension(northward movement) of the South Asian High(Atlantic Intertropical Convergence Zone), and exerts strong impacts on upstream climate variations from North Atlantic to West Asia. It also affects oceanic circulation and buoyancy fields via atmospheric stationary wave trains and air–sea interaction processes, contributing to formation of the Atlantic Meridional Overturning Circulation. The TP thermal state and atmospheric–oceanic conditions are highly interactive and Asian summer monsoon variability is controlled synergistically by internal TP variability and external forcing factors.

引用

页码：534 / 552

页数：19

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