摘要 : The summer intraseasonal oscillation (ISO) is characterized by a northward-moving rainband in the Indo-western Pacific warm pool region. The physical origin of the ISO is not fully understood, as it is masked by strong interaction... 展开 The summer intraseasonal oscillation (ISO) is characterized by a northward-moving rainband in the Indo-western Pacific warm pool region. The physical origin of the ISO is not fully understood, as it is masked by strong interaction of convection and circulation. This study examines intraseasonal to interannual variability during June-August over the Indo-western Pacific warm pool region. The results show that the tropical northwest Pacific anomalous anticyclone (NWP-AAC) is a fundamental mode on both intraseasonal and interannual time scales, destabilized by the monsoon mean state, specifically through barotropic energy conversion and convective feedback in the low-level confluence between the monsoon westerlies and easterly trade winds. On the interannual time scale, the NWP-AAC shows a biennial tendency, reversing phase from the summer of El Nino to the summer that follows; the AAC in post-El Milo summer is excited indirectly through sea surface temperature anomalies in the Indo-NWP. On the intraseasonal time scale, the column-integrated moisture advection causes the NWP-AAC-related convection to propagate northward. Our results provide a unifying view of multiscale Asian summer monsoon variability, with important implications for subseasonal to seasonal prediction. 收起