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A decadal change has occurred on the relationship between the summertime western North Pacific subtropical High (WNPSH) and the tropical Sea Surface Temperature anomalies (SSTA) in the early 1990s. After this decadal change, the interannual variability of the WNPSH is more strongly regulated by the SSTA over the equatorial central Pacific and the maritime continent. The earlier decay of El Niño in...
The direct effect of lower‐tropospheric diabatic heating (DH) on surface circulation over the equatorial Pacific is revealed using the theoretical analysis and three atmospheric general circulation model (AGCM) simulations, only differing their moist processes. The AGCM results suggest that the insensitivity of surface wind to DH in the middle and high levels is closely associated with the vertical...
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