Physics
Scientific paper
Dec 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29x..46s&link_type=abstract
Geophysical Research Letters, Volume 29, Issue 24, pp. 46-1, CiteID 2193, DOI 10.1029/2002GL016144
Physics
15
Meteorology And Atmospheric Dynamics: Paleoclimatology
Scientific paper
Using a box model of the North Atlantic Ocean and a parameterization of Heinrich Events, we suggest that self-sustained oscillations of the large-scale oceanic circulation provide a framework to accommodate crucial elements of late Pleistocene climate variability: (i) Dansgaard-Oeschger-style oscillations with varying interstadial length, (ii) synchronization between Dansgaard-Oeschger stadials and Heinrich Events, and (iii) Younger Dryas-type events. The latter result from the restart of the oscillations after a glacial maximum and can be regarded as Dansgaard-Oeschger stadials, overprinted by rapidly changing boundary conditions.
Paul André
Schulz Michael
Timmermann Axel
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