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DOI10.1126/science.1104666
Cool La Niña during the warmth of the Pliocene?
Rickaby R.E.M.; Halloran P.
发表日期2005
ISSN0036-8075
起始页码1948
结束页码1952
卷号307期号:5717
英文摘要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.
英文关键词Greenhouse effect; Oceanography; Oscillations; Temperature distribution; Cold upwelling; Pliocene; Surface temperature gradient; Thermocline tilt; Global warming; calcium; magnesium; oxygen 18; sea water; surface water; La Nina; paleoclimate; Pliocene; article; calcification; climate change; cooling; El Nino; environmental temperature; greenhouse effect; heating; hydrography; la nina; Pacific Ocean; paleoceanography; paleoclimate; plankton; Pliocene; priority journal; salinity; thermocline
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245218
作者单位Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, United Kingdom
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Rickaby R.E.M.,Halloran P.. Cool La Niña during the warmth of the Pliocene?[J],2005,307(5717).
APA Rickaby R.E.M.,&Halloran P..(2005).Cool La Niña during the warmth of the Pliocene?.Science,307(5717).
MLA Rickaby R.E.M.,et al."Cool La Niña during the warmth of the Pliocene?".Science 307.5717(2005).
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