Global Monsoon Dynamics and Climate Change

被引：412

作者：

An Zhisheng ^{[1
,3
]}

Wu Guoxiong ^{[2
]}

Li Jianping ^{[2
,4
,5
]}

Sun Youbin ^{[1
]}

Liu Yimin ^{[2
]}

Zhou Weijian ^{[1
]}

Cai Yanjun ^{[1
]}

Duan Anmin ^{[2
]}

Li Li ^{[1
]}

Mao Jiangyu ^{[2
]}

Cheng Hai ^{[3
,6
]}

Shi Zhengguo ^{[1
]}

Tan Liangcheng ^{[1
]}

Yan Hong ^{[1
]}

Ao Hong ^{[1
]}

Chang Hong ^{[1
]}

Feng Juan ^{[2
]}

机构：

[1] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China

[2] Chinese Acad Sci, State Key Lab Numer Modeling Atmospher Sci & Geop, Inst Atmospher Phys, Beijing 100029, Peoples R China

[3] Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China

[4] Beijing Normal Univ, Coll Global Change & Earth Syst Sci GCESS, Beijing 100875, Peoples R China

[5] Joint Ctr Global Change Studies, Beijing 100875, Peoples R China

[6] Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA

来源：

ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 43 | 2015年 / 43卷

关键词：

global monsoon; monsoon dynamics; climate change; multitimescale; paleomonsoon; Tibetan Plateau; Asian monsoon; monsoon variability; monsoon characteristics; land-air sea interaction; insolation; surface boundary conditions; monsoon definition; ASIAN SUMMER MONSOON; SOUTH CHINA SEA; SURFACE TEMPERATURE VARIABILITY; INTERTROPICAL CONVERGENCE ZONE; LOESS-PALEOSOL SEQUENCES; EQUATORIAL EAST-AFRICA; LATE CENOZOIC UPLIFT; NORTH-CENTRAL CHINA; TIBETAN PLATEAU; INDIAN MONSOON;

D O I：

10.1146/annurev-earth-060313-054623

中图分类号：

P1 [天文学];

学科分类号：

0704 ;

摘要：

This article provides a comprehensive review of the global monsoon that encompasses findings from studies of both modern monsoons and paleomonsoons. We introduce a definition for the global monsoon that incorporates its three-dimensional distribution and ultimate causes, emphasizing the direct drive of seasonal pressure system changes on monsoon circulation and depicting the intensity in terms of both circulation and precipitation. We explore the global monsoon climate changes across a wide range of timescales from tectonic to intraseasonal. Common features of the global monsoon are global homogeneity, regional diversity, seasonality, quasi-periodicity, irregularity, instability, and asynchroneity. We emphasize the importance of solar insolation, Earth orbital parameters, underlying surface properties, and land-air-sea interactions for global monsoon dynamics. We discuss the primary driving force of monsoon variability on each timescale and the relationships among dynamics on multiple timescales. Natural processes and anthropogenic impacts are of great significance to the understanding of future global monsoon behavior.

引用

页码：29 / 77

页数：49

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