The DOI matches its Crossref record; 25 of the 25 references it cites were found in a registry or an index.
Permanent El Niño-Like Conditions During the Pliocene Warm Period
Abstract
During the warm early Pliocene (∼4.5 to 3.0 million years ago), the most recent interval with a climate warmer than today, the eastern Pacific thermocline was deep and the average west-to-east sea surface temperature difference across the equatorial Pacific was only 1.5 ± 0.9°C, much like it is during a modern El Niño event. Thus, the modern strong sea surface temperature gradient across the equatorial Pacific is not a stable and permanent feature. Sustained El Niño-like conditions, including relatively weak zonal atmospheric (Walker) circulation, could be a consequence of, and play an important role in determining, global warmth.
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Cites
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Self-citationCore top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation
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Jackson, J. B. C. (2008) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0802812105 · Cited by 611
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Wang, P. X., Wang, B., Cheng, H., Fasullo, J., Guo, Z., Kiefer, T., & Liu, Z. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.07.006 · Cited by 508
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Metadata
- Authors
- Wara, M. W., Ravelo, A. C., & Delaney, M. L.
- Venue
- Science
- Published
- 2005-07-29
- Volume
- 309
- Issue
- 5735
- Pages
- 758-761
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2006547330
- Cited by
- 674
- References
- 25
- FWCI
- 14.28
- Type
- journal article
- Language
- en
- Open access
- closed
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