It has been found that the warm sea surface temperature anomaly in the Antarctic Circumpolar Current (ACC) propagates eastward at a 4-5 year period circling Antarctica. It also stretches northeastward across most of the subtropical South Pacific. Part of it turns north branching off into Peru Current where happened to be El Nino birth place. Is this warm anomaly originated from the ACC a possible triggering cause of the onset of an El Nino event?
A recent study validated the ability of NCAR Climate System Model (CSM)in capturing El Nino time scale variations (Liang,1998). The results from fully coupled CSM experiments provide us better data to examine our hypothesis that links tropical Pacific El Nino to Antarctic Circumpolar Wave. We re-examine El Nino signals in southern oceans in the NCAR CSM 300-year fully coupled simulation and further explore evidences that links Antarctic Circumpolar Wave to El Nino onset from the NCAR CSM 1870-1998's historical simulation.