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Glacial-Interglacial Indian Summer Monsoon Dynamics

Zhisheng, An ; Clemens, Steven C. ; Shen, Ji ; Qiang, Xiaoke ; Jin, Zhangdong ; Sun, Youbin ; Prell, Warren L. ; Luo, Jingjia ; Wang, Sumin ; Xu, Hai ; Cai, Yanjun ; Zhou, Weijian ; Liu, Xiaodong ; Liu, Weiguo ; Shi, Zhengguo ; Yan, Libin ; Xiao, Xiayun ; Chang, Hong ; Wu, Feng ; Ai, Li ; Lu, Fengyan

Science (American Association for the Advancement of Science), 2011-08, Vol.333 (6043), p.719-723 [Periódico revisado por pares]

Washington, DC: American Association for the Advancement of Science

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Título:
Glacial-Interglacial Indian Summer Monsoon Dynamics
Autor: Zhisheng, An ; Clemens, Steven C. ; Shen, Ji ; Qiang, Xiaoke ; Jin, Zhangdong ; Sun, Youbin ; Prell, Warren L. ; Luo, Jingjia ; Wang, Sumin ; Xu, Hai ; Cai, Yanjun ; Zhou, Weijian ; Liu, Xiaodong ; Liu, Weiguo ; Shi, Zhengguo ; Yan, Libin ; Xiao, Xiayun ; Chang, Hong ; Wu, Feng ; Ai, Li ; Lu, Fengyan
Assuntos: Atmospheric circulation ; Atmospheric sciences ; Climate ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Glaciers ; Ice ; In kind support and maintenance ; Marine and continental quaternary ; Mathematical maxima ; Mathematical minima ; Monsoons ; Musical intervals ; Oceans ; Proxy reporting ; Proxy statements ; Summer ; Surficial geology ; Wind
É parte de: Science (American Association for the Advancement of Science), 2011-08, Vol.333 (6043), p.719-723
Notas: ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
Descrição: 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.
Editor: Washington, DC: American Association for the Advancement of Science
Idioma: Inglês

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Glacial-Interglacial Indian Summer Monsoon Dynamics

Washington, DC: American Association for the Advancement of Science

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