摘要 : While enhanced rainbands progressed northward in East Asia from June to August during the regular El Nino decaying summer, strengthened rainbands were only observed in the earlier summer and disappeared in August in the super El N... 展开 While enhanced rainbands progressed northward in East Asia from June to August during the regular El Nino decaying summer, strengthened rainbands were only observed in the earlier summer and disappeared in August in the super El Nino composite. The cause of this distinctive feature is investigated through a combined observational and modeling study. The relative roles of the mean state and anomalous heating in causing the northward progression in the regular El Nino group are assessed through idealized numerical experiments. The result shows that the monthly evolving mean state is more important, while the anomalous forcing also plays a role. The distinctive rainfall feature in the super El Nino composite was primarily contributed by the 1982/83 and 2015/16 events, whereas the rainband evolution in 1998 resembled the regular El Nino composite. The cause of the different rainfall pattern in August among the super El Nino events is further investigated. A marked difference exists in the tropical sea surface temperature anomaly (SSTA) and associated anomalous precipitation patterns. A low-level cyclonic (anticyclonic) anomaly appeared south of Japan in August 1983 and 2016 (1998), inducing northerly (southerly) anomalies and thus suppressed (enhanced) rainfall in eastern China. Whereas an anomalous anticyclone in the western North Pacific (WNP) is a typical response to an El Nino during its mature and decaying phases, the formation of a cyclonic anomaly in the WNP resulted from anomalous enthalpy advection associated with the eastward retreat of an anomalous anticyclone triggered by a local cold SSTA belt in August 1983 and from a Pacific meridional mode (PMM)-like positive SSTA pattern in August 2016. 收起