Glacial-Interglacial Indian Summer Monsoon Dynamics

被引：455

作者：

An Zhisheng ^{[1
,2
]}

Clemens, Steven C. ^{[3
]}

Shen, Ji ^{[4
]}

Qiang, Xiaoke ^{[1
]}

Jin, Zhangdong ^{[1
]}

Sun, Youbin ^{[1
]}

Prell, Warren L. ^{[3
]}

Luo, Jingjia ^{[5
]}

Wang, Sumin ^{[4
]}

Xu, Hai ^{[1
]}

Cai, Yanjun ^{[1
]}

Zhou, Weijian ^{[1
,2
]}

Liu, Xiaodong ^{[1
]}

Liu, Weiguo ^{[1
]}

Shi, Zhengguo ^{[1
]}

Yan, Libin ^{[1
]}

Xiao, Xiayun ^{[4
]}

Chang, Hong ^{[1
]}

Wu, Feng ^{[1
]}

Ai, Li ^{[1
]}

Lu, Fengyan ^{[1
]}

机构：

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

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

[3] Brown Univ, Dept Geol Sci, Providence, RI 02912 USA

[4] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China

[5] Japan Agcy Marine Earth Sci & Technol, Res Inst Global Change, Kanagawa 2360001, Japan

来源：

SCIENCE | 2011年 / 333卷 / 6043期

基金：

中国国家自然科学基金;

关键词：

CLIMATE SIMULATION; VARIABILITY; HOLOCENE; HISTORY; RECORD; EVOLUTION; MAXIMUM; CORE;

D O I：

10.1126/science.1203752

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

The modern Indian summer monsoon (ISM) is characterized by exceptionally strong interhemispheric transport, indicating the importance of both Northern and Southern Hemisphere processes driving monsoon variability. Here, we present a high-resolution continental record from southwestern China that demonstrates the importance of interhemispheric forcing in driving ISM variability at the glacial-interglacial time scale as well. Interglacial ISM maxima are dominated by an enhanced Indian low associated with global ice volume minima. In contrast, the glacial ISM reaches a minimum, and actually begins to increase, before global ice volume reaches a maximum. We attribute this early strengthening to an increased cross-equatorial pressure gradient derived from Southern Hemisphere high-latitude cooling. This mechanism explains much of the nonorbital scale variance in the Pleistocene ISM record.

引用

页码：719 / 723

页数：5

共 55 条

[11] Dust response to seasonal atmospheric forcing: Proxy evaluation and calibration [J].

Clemens, SC .

PALEOCEANOGRAPHY, 1998, 13 (05) :471-490

[12] A 350,000 year summer-monsoon multi-proxy stack from the Owen ridge, Northern Arabian sea [J].

Clemens, SC ;

Prell, WL .

MARINE GEOLOGY, 2003, 201 (1-3) :35-51

[13] Southern Hemisphere forcing of Pliocene δ18O and the evolution of Indo-Asian monsoons [J].

Clemens, Steven C. ;

Prell, Warren L. ;

Sun, Youbin ;

Liu, Zhengyu ;

Chen, Guangshan .

PALEOCEANOGRAPHY, 2008, 23 (04)

[14]

Farjon A, 1990, PINACEAE DRAWINGS DE, P149

[15] Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra) [J].

Fleitmann, Dominik ;

Burns, Stephen J. ;

Mangini, Augusto ;

Mudelsee, Manfred ;

Kramers, Jan ;

Villa, Igor ;

Neff, Ulrich ;

Al-Subbary, Abdulkarim A. ;

Buettner, Annett ;

Hippler, Dorothea ;

Matter, Albert .

QUATERNARY SCIENCE REVIEWS, 2007, 26 (1-2) :170-188

[16] On the age of the Laschamp geomagnetic excursion [J].

Guillou, H ;

Singer, BS ;

Laj, C ;

Kissel, C ;

Scaillet, S ;

Jicha, BR .

EARTH AND PLANETARY SCIENCE LETTERS, 2004, 227 (3-4) :331-343

[17] Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean [J].

Gupta, AK ;

Anderson, DM ;

Overpeck, JT .

NATURE, 2003, 421 (6921) :354-357

[18] Paleoclimate of Southwestern China for the past 50,000 yr inferred from lake sediment records [J].

Hodell, DA ;

Brenner, M ;

Kanfoush, SL ;

Curtis, JH ;

Stoner, JS ;

Song, XL ;

Yuan, W ;

Whitmore, TJ .

QUATERNARY RESEARCH, 1999, 52 (03) :369-380

[19]

HOLTON JR, 1992, INTRO DYNAMIC METEOR, P310

[20]

Imbrie J., 1984, Milankovitch and Climate: Understanding the Response to Astronomical Forcing, -, V1, P269

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