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- W2012365214 abstract "During the latter half of the Cenozoic, starting during the Pliocene, the eastern equatorial Pacific (EEP) underwent a change from warm, wet climate conditions—which scientists refer to as “permanent El Nino”—to more moderate conditions like those observed today. Although scientists can track this change using marine proxy records, they are still puzzled as to why the sudden shift occurred." @default.
- W2012365214 created "2016-06-24" @default.
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- W2012365214 date "2014-11-04" @default.
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- W2012365214 title "Peruvian Andes helped to cool eastern equatorial Pacific" @default.
- W2012365214 doi "https://doi.org/10.1002/2014eo440013" @default.
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