Prior to the 1976-77 climate shift (1950-76), sea surface temperature (SST) anomalies in the tropical Indian Ocean consisted of a basinwide warming during boreal fall of the developing phase of most El Ni (n) over tilde os, whereas after the shift (1977-99) they had an east-west asymmetry-a consequence of El Ni (n) over tildeo being associated with the Indian Ocean Dipole/Zonal mode. In this study, the possible impact of these contrasting, SST patterns on the ongoing El Ni (n) over tildeo is investigated, using atmospheric reanalysis products and solutions to both an atmospheric general circulation model (AGCM) and a simple atmospheric model (LBM), with the latter used to identify basic processes. Specifically, analyses of reanalysis products during the El Ni (n) over tildeo onset indicate that after the climate shift a low-level anticyclone over the South China Sea was shifted into the Bay of Bengal and that equatorial westerly anomalies in the Pacific Ocean were considerably stronger. The present study focuses on determining influence of Indian Ocean SST on these changes. A suite of AGCM experiments, each consisting of a 10-member ensemble, is carried out to assess the relative importance of remote (Pacific) versus local (Indian Ocean) SST anomalies in determining precipitation anomalies over the equatorial Indian Ocean. Solutions indicate that both local and remote SST anomalies are necessary for realistic simulations with convection in the tropical west Pacific and the subsequent development of the South China Sea anticyclone being particularly sensitive to Indian Ocean SST anomalies. Prior to the climate shift, the basinwide Indian Ocean SST anomalies generate an atmospheric Kelvin wave associated with easterly flow over the equatorial west-central Pacific, thereby weakening the westerly anomalies associated with the developing El Ni (n) over tildeo. In contrast, after the shift, the east-west contrast in Indian Ocean SST anomalies does not generate a significant Kelvin wave response, and there is little effect on the El Ni (n) over tildeo-induced westerlies. The Linear Baroclinic Model (LBM) solutions confirm the AGCM's results.
