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Review
. 2018 Jul;559(7715):535-545.
doi: 10.1038/s41586-018-0252-6. Epub 2018 Jul 25.

El Niño-Southern Oscillation complexity

Affiliations
Review

El Niño-Southern Oscillation complexity

Axel Timmermann et al. Nature. 2018 Jul.

Erratum in

  • Author Correction: El Niño-Southern Oscillation complexity.
    Timmermann A, An SI, Kug JS, Jin FF, Cai W, Capotondi A, Cobb KM, Lengaigne M, McPhaden MJ, Stuecker MF, Stein K, Wittenberg AT, Yun KS, Bayr T, Chen HC, Chikamoto Y, Dewitte B, Dommenget D, Grothe P, Guilyardi E, Ham YG, Hayashi M, Ineson S, Kang D, Kim S, Kim W, Lee JY, Li T, Luo JJ, McGregor S, Planton Y, Power S, Rashid H, Ren HL, Santoso A, Takahashi K, Todd A, Wang G, Wang G, Xie R, Yang WH, Yeh SW, Yoon J, Zeller E, Zhang X. Timmermann A, et al. Nature. 2019 Mar;567(7746):E3. doi: 10.1038/s41586-019-0994-9. Nature. 2019. PMID: 30787440

Abstract

El Niño events are characterized by surface warming of the tropical Pacific Ocean and weakening of equatorial trade winds that occur every few years. Such conditions are accompanied by changes in atmospheric and oceanic circulation, affecting global climate, marine and terrestrial ecosystems, fisheries and human activities. The alternation of warm El Niño and cold La Niña conditions, referred to as the El Niño-Southern Oscillation (ENSO), represents the strongest year-to-year fluctuation of the global climate system. Here we provide a synopsis of our current understanding of the spatio-temporal complexity of this important climate mode and its influence on the Earth system.

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References

    1. Carrillo, C. N. Hidrografía oceánica. Bol. Soc. Geogr. Lima 1, 72–110 (1893).
    1. Bjerknes, J. Atmospheric teleconnections from the equatorial Pacific. Mon. Weath. Rev. 97, 163–172 (1969).
    1. McPhaden, M. J., Busalacchi, A. J. & Anderson, D. L. T. A TOGA retrospective. Oceanography 23, 86–103 (2010).
    1. Cai, W. J. et al. More extreme swings of the South Pacific convergence zone due to greenhouse warming. Nature 488, 365–369 (2012). - PubMed
    1. Capotondi, A. et al. Understanding ENSO diversity. Bull. Am. Meteorol. Soc. 96, 921–938 (2015).

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