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Palaeoclimate reconstructions reveal a strong link between El Niño-Southern Oscillation and Tropical Pacific mean state

Sadekov, A.Y.; Ganeshram, R.; Pichevin, L.; Berdin, R.; McClymont, E.L.; Elderfield, H.; Tudhope, A.W.

Palaeoclimate reconstructions reveal a strong link between El Niño-Southern Oscillation and Tropical Pacific mean state Thumbnail


Authors

A.Y. Sadekov

R. Ganeshram

L. Pichevin

R. Berdin

H. Elderfield

A.W. Tudhope



Abstract

The El Niño-Southern Oscillation (ENSO) is one of the most important components of the global climate system, but its potential response to an anthropogenic increase in atmospheric CO2 remains largely unknown. One of the major limitations in ENSO prediction is our poor understanding of the relationship between ENSO variability and long-term changes in Tropical Pacific oceanography. Here we investigate this relationship using palaeorecords derived from the geochemistry of planktonic foraminifera. Our results indicate a strong negative correlation between ENSO variability and zonal gradient of sea-surface temperatures across the Tropical Pacific during the last 22 ky. This strong correlation implies a mechanistic link that tightly couples zonal sea-surface temperature gradient and ENSO variability during large climate changes and provides a unique insight into potential ENSO evolution in the future by suggesting enhanced ENSO variability under a global warming scenario.

Citation

Sadekov, A., Ganeshram, R., Pichevin, L., Berdin, R., McClymont, E., Elderfield, H., & Tudhope, A. (2013). Palaeoclimate reconstructions reveal a strong link between El Niño-Southern Oscillation and Tropical Pacific mean state. Nature Communications, 4(11), Article 2692. https://doi.org/10.1038/ncomms3692

Journal Article Type Article
Publication Date Nov 1, 2013
Deposit Date Oct 9, 2013
Publicly Available Date Mar 29, 2024
Journal Nature Communications
Publisher Nature Research
Peer Reviewed Peer Reviewed
Volume 4
Issue 11
Article Number 2692
DOI https://doi.org/10.1038/ncomms3692

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