Modeling climate shift of El Nino variability in the holocene

Details Modeling climate shift of El Nino variability in the holocene Modeling climate shift of El Nino variability in the holocene

Aug 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000georl..27.2265l&link_type=abstract

Geophysical Research Letters, Volume 27, Issue 15, p. 2265-2268

Physics

94

Meteorology And Atmospheric Dynamics: Ocean/Atmosphere Interactions, Meteorology And Atmospheric Dynamics: Paleoclimatology

Scientific paper

A coupled ocean-atmosphere general circulation model is used to investigate climatic shift of El Nino in the Holocene. The model simulates a reduced ENSO intensity in the early and mid-Holocene, in agreement with paleoclimate record. The ENSO reduction is proposed to be caused by both an intensified Asian summer monsoon and a warm water subduction from the South Pacific into the equatorial thermocline.

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