Heinrich event 1: an example of dynamical ice-sheet reaction to oceanic changes

Heinrich events, identified as enhanced ice-rafted detritus (IRD) in North Atlantic deep sea sediments (Heinrich, 1988; Hemming, 2004) have classically been attributed to Laurentide ice-sheet (LIS) instabilities (MacAyeal, 1993; Calov et al., 2002; Hulbe et al., 2004) and assumed to lead to importan...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Álvarez-Solas, J., Montoya, M., Ritz, C., Ramstein, G., Charbit, S., Dumas, C., Nisancioglu, K., Dokken, T., Ganopolski, A.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/cp-7-1297-2011
https://noa.gwlb.de/receive/cop_mods_00026504
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026459/cp-7-1297-2011.pdf
https://cp.copernicus.org/articles/7/1297/2011/cp-7-1297-2011.pdf