Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
Science Signaling

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 25 March 2005:
Vol. 307. no. 5717, pp. 1948 - 1952
DOI: 10.1126/science.1104666
Prev | Table of Contents | Next

Reports

Cool La Niña During the Warmth of the Pliocene?

R. E. M. Rickaby and P. Halloran

The role of El Niño–Southern Oscillation (ENSO) in greenhouse warming and climate change remains controversial. During the warmth of the early-mid Pliocene, we find evidence for enhanced thermocline tilt and cold upwelling in the equatorial Pacific, consistent with the prevalence of a La Niña–like state, rather than the proposed persistent warm El Niño–like conditions. Our Pliocene paleothermometer supports the idea of a dynamic "ocean thermostat" in which heating of the tropical Pacific leads to a cooling of the east equatorial Pacific and a La Niña–like state, analogous to observations of a transient increasing east-west sea surface temperature gradient in the 20th-century tropical Pacific.

Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK.

Read the Full Text

ADVERTISEMENT
Click Me!

ADVERTISEMENT
Click Me!

To Advertise     Find Products

Science. ISSN 0036-8075 (print), 1095-9203 (online)