LAUSR

AbstractPresent study documents the biases of summertime northwest Pacific (NWP) atmospheric circulation anomalies during the decaying phase of ENSO and investigates their plausible reasons in 32 Coupled Model Intercomparison Project phase 5 models. Based on an inter-model empirical orthogonal function (EOF) analysis of El Nino-Southern Oscillation (ENSO)-related 850hPa wind anomalies, the dominant modes of biases are extracted. The first EOF mode, explaining 21.3% of total inter-model variance, is characterized by a cyclone over the NWP, indicating a weaker NWP anticyclone. The cyclone appears to be a Rossby wave response to unrealistic equatorial western Pacific (WP) sea surface temperature (SST) anomalies related to excessive equatorial Pacific cold tongue in the models. On one hand, the cold SST biases increase the mean zonal SST gradient, which further intensifies warm zonal advection, favoring the development and persistence of equatorial WP SST anomalies. On the other hand, they reduce the anomalou...