首页> 中文会议>中国地球物理学会第二十九届年会 >晚中新世至上新世东亚夏季风加强与南半球冰量增加的联系

晚中新世至上新世东亚夏季风加强与南半球冰量增加的联系

摘要

The Asian monsoon system represents one of the most dynamic interactions of thecontinent-ocean-atmosphere systems on the globe.It controls much of the Asian climate variations.Particularly,the monsoon-associated precipitation forms a basis of how to manage impacts on the environmentand to organize societal and economic activities in the densely populated Asia.Climate model experimentshave suggested that uplift of the Tibetan Plateau and retreat of the Paratethys sea in western Asia associatedwith the Indo-Asia collision during the Cenozoic era can result in monsoon intensification.

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