El Niño–Southern Oscillation, Pliocene climate and equifinality
El Niño–Southern Oscillation, Pliocene climate and equifinality
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Publisher
London: The Royal Society
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Language
English
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Publisher
London: The Royal Society
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Contents
It has been suggested that, during the Pliocene (ca 5-1.8 Ma), an El Niño state existed as a permanent rather than an intermittent feature; that is, the tropical Pacific Ocean was characterized by a much weaker east-west gradient than today. One line of inquiry used to investigate this idea relates modern El Niño teleconnections to Pliocene proxy d...
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Full title
El Niño–Southern Oscillation, Pliocene climate and equifinality
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TN_cdi_jstor_primary_40485430
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_jstor_primary_40485430
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ISSN
1364-503X
E-ISSN
1471-2962
DOI
10.1098/rsta.2008.0212
