Abstract:An index of El Niño Southern Oscillation (ENSO) in the Pacific during February through April is shown to account for a significant part of the variability of coastal sea surface temperature (SST) anomalies measured a few months later within the central east coast of India (CEI). This ENSO-related modulation of coastal upwelling appears to contribute to the connection observed at the basin-scale between ENSO and SST in the Bay of Bengal. The ability to use this teleconnection to give warning of large changes in… Show more
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