Abstract
A near-annual coupled ocean-atmosphere mode in the equatorial Pacific is studied using the NCEP ocean assimilation data set. This fast mode of tropical Pacific climate variability is superimposed on the slow 3-5 year El Niño-Southern Oscillation (ENSO) phenomenon. Anomalous zonal advection plays a crucial role in generating this fast mode. It is suggested that this fast mode can be understood in terms of a coupled Pacific basin mode. It is responsible for the occurrence of some minor El Niño and La Niña events and has implications for the prediction of ENSO events.
Original language | English |
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Pages (from-to) | 52-1 - 52-4 |
Journal | Geophysical Research Letters |
Volume | 30 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2003 Jan 15 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Earth and Planetary Sciences(all)