Changes in North Atlantic deep-water formation associated with the Dansgaard–Oeschger temperature oscillations (60–10 ka)

By M. Elliot, L. Labeyrie, J. Duplessy. 2002

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Large‐scale instabilities of the Laurentide ice sheet simulated in a fully coupled climate‐system model (2002, background): “There is a growing body of evidence that indicates that HEs not only represent catastrophic glaciological events, but also that they are closely related to abrupt climate changes [Bard et al., 2000] via considerable slowdown of the Atlantic thermohaline circulation [Elliot et al., 2002].”
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes (2004, background): “, and diminished relative influence of northern-source deep waters during that tim”
Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing (2013, background): “According to these marine records and other data sets from the northern North Atlantic (e.g.,Elliot et al., 1998; Grousset et al. , 2001; Elliot et al., 2002), the iceberg calving increased during interstadial periods and peaked at the end of the stadials, after which it decayed rapidly.”