Distinct Evolution of Sea Surface Temperature over the Cold Tongue Region in South China Sea during Various El Nino Events

This study investigates the evolution of the sea surface temperature (SST) over the cold tongue (CT) region in the central South China Sea (SCS) during various El Nino events. A significant and distinct double-peak warming evolution can occur during EP El Nino and CP El Nino events, with the former being more remarkable and robust than the latter. Further analyses show that the weak and insignificant CT SST anomaly in CP El Nino events is influenced by some CP El Nino events in which the warm sea surface temperature anomaly (SSTA) is located west of 175 degrees E (WCP El Nino). The response of CT SSTA mainly depends on the warm SSTA location of CP El Nino. The different corresponding mechanisms in winter, spring and summer are discussed respectively in this work. Further analysis reveals that the weak and insignificant SST anomaly over the CT region in CP El Nino events is caused by the faint SSTA response during the WCP El Nino events. The results of this study call attention to the response of the SCS climate in both atmosphere and ocean to the diversity of ENSO, especially the CP El Nino.