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, Jorge, 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 Gesellschaft MBH 2011
Subjects:
Online Access:https://eprints.ucm.es/id/eprint/24248/
https://eprints.ucm.es/id/eprint/24248/1/alvarezsolas05libre.pdf
https://doi.org/10.5194/cp-7-1297-2011