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Advances in Geosciences An open-access journal for refereed proceedings and special publications
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Volume 6
Adv. Geosci., 6, 3–15, 2006
https://doi.org/10.5194/adgeo-6-3-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Adv. Geosci., 6, 3–15, 2006
https://doi.org/10.5194/adgeo-6-3-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  09 Jan 2006

09 Jan 2006

The ENSO phenomenon: theory and mechanisms

H. A. Dijkstra H. A. Dijkstra
  • Institute for Marine and Atmospheric Research, Dept. of Physics and Astronomy, Utrecht University, The Netherlands

Abstract. The variability in the equatorial Tropical Pacific is characterized by sea-surface temperature anomalies and associated changes in the atmospheric circulation. Through an enormous monitoring effort over the last decades, the relevant time scales and spatial patterns are fairly well-documented. In the meantime, a hierarchy of models has been developed to understand the physics of this phenomenon and to make predictions of future variability. In this short review, I try to summarize theories and mechanisms about variability in such a way that these are accessible to a diverse group of researchers, such as that present in Guayaquil (in May 2005) at the First International Alexander Von Humboldt Conference "The El Niño Phenomenon and its Global Impact".

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