• 责任者：Shi Zhengguo (Institute of Earth Environment ; Chinese Academy of Sciences ; Xi’an 710075 ; China) ; Liu Xiaodong
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2009
• 卷期：29(5)
• 关键词：全新世 ; Holocene ; 古季风 ; 东亚 ; Eastern Asia ; 南亚 ; Southern Asia
• 页码：p.83-88
• 图表：4 illus., 31 refs.
• 分类号：1400
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

Recent studies indicate the inverse phase relation between East Asian and South Asian summer monsoons on the interannual scale. In this paper, NCEP/NCAR data and outputs from GCM transient simulation are analyzed to further appeal that the relation might also exist on the orbital scale and it well links with the Paleo-ENSO evolution. During the El Niñ-like conditions, the East Asian summer monsoon is strengthened but the South Asian one is decreased. However, these responses are distinctly inverse when the La Niñ-like events occur. The similar responses of monsoon systems on different time scales could provide better explanations for our geological records.