摘要
This study discusses the potential contribution of the Pacific decadal oscillation(PDO)to the weakening of the East Asian summer monsoon(EASM)and the evident correlation between the positive PDO and"Southern flood and Northern drought(SFND)"summer rainfall pattern over East China.The mechanism behind this contribution is also discussed.
This study discusses the potential contribution of the Pacific decadal oscillation （PDO） to the weakening of the East Asian summer monsoon （EASM） and the evident correlation between the positive PDO and ＂Southern flood and Northern drought （SFND）＂ summer rainfall pattern over East China.The mechanism behind this contribution is also discussed.
基金
supported by the National Basic Research Program of China(Grant No.2009CB421401)
the Research Council of Norway through the DecCen project(Exploring Decadal to Century Scale Variability and Changes in the East Asian Climate during the last Millennium)
