Abstract
AbstractAn 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 the CEI a few months in advance is exemplified using data 1998–1999 ENSO events. Copyright © 2008 Royal Meteorological Society
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
