El Niño Dynamics
DOI: 10.1063/1.882496
The El Niño/Southern Oscillation phenomenon (ENSO, for short) is the strongest source of natural variability in Earth’s climate system. Although ENSO originates in the tropical latitudes of the Pacific Ocean, its climatic impact is felt globally. Variations in major rainfall systems that are attributed to ENSO range from droughts in Indonesia and Australia to storms and flooding in Ecuador and the US.
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References
1. S. G. H. Philander, El Niño. La Niña, and the Southern Oscillation, Academic Press, San Diego, Calif. (1990).
See also review articles on ENSO in J. Geophys. Res., 103, 14167 (1998).https://doi.org/JGREA22. J. M. Wallace et al., J. Geophys. Res. 103, 14241 (1998). https://doi.org/JGREA2
K. E. Trenberth et al., J. Geophys. Res. 103, 14291 (1998). https://doi.org/JGREA2
P. J. Webster et al., J. Geophys. Res. 103, 14451 (1998).https://doi.org/JGREA23. M. J. McFadden et al., J. Geophys. Res. 103, 14169 (1998).https://doi.org/JGREA2
4. J. D. Neelin et al., J. Geophys. Res. 103, 14261 (1998). https://doi.org/JGREA2
T. N. Stockdale et al., J. Geophys. Res. 103, 14325 (1998). https://doi.org/JGREA2
P. Delecluse et al., J. Geophys. Res. 103, 14357 (1998).https://doi.org/JGREA25. M. Latif et al., J. Geophys. Res. 103, 14375 (1998).https://doi.org/JGREA2
More about the Authors
J. David Neelin. University of California, Los Angeles.
Mojib Latif. Max Planck Institute for Meteorology, Hamburg, Germany.
