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...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2011
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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 |