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A Mechanism for Explaining the Maximum Intraseasonal Oscillation Center over the Western North Pacific*
Journal of Climate
During late boreal summer (July-October), the intraseasonal oscillation (ISO) exhibits maximum variability over the western North Pacific (WNP) centered in the South China Sea and Philippine Sea, but many numerical models have difficulty in simulating this essential feature of the ISO. To understand why this maximum variability center exists, the authors advance a simple box model to elaborate the potential contribution of the mean-state-dependent atmosphere-ocean interaction. The model resultsdoi:10.1175/jcli-d-12-00797.1 fatcat:5ahf4hzqyfdpjej4devnvnqily