ENSO, Climate Variability, and the Rapanui: Part 2. Oceanography and Rapa Nui

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dc.contributor.authorMacIntyre, Ferren
dc.date.accessioned2021-11-12T21:52:24Z
dc.date.available2021-11-12T21:52:24Z
dc.date.issued2001-01-01
dc.description.abstract<p>The metronome of ENSO is the steady eastward drift of equatorial atmospheric convection centers. The natural position of a convection center is over the warmest water; drift displaces it (and the warmest water) in a quasi-regular manner. When it is far enough downstream, a new center regenerates in its home position, beginning the cycle again.</p>
dc.identifier.urihttp://hdl.handle.net/10524/64514
dc.subjectRapa Nui
dc.subjectEaster Island
dc.subjectClimate
dc.titleENSO, Climate Variability, and the Rapanui: Part 2. Oceanography and Rapa Nui
dc.title.alternativeENSO, Climate Variability, and the Rapanui: Part 2
dc.typeResearch paper
dc.type.dcmiText
prism.number2
prism.volume15

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Rapa Nui Journal Volume 15 Issue 2