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Absence of Cooling in New Zealand and the Adjacent Ocean During the Younger Dryas Chronozone

Barrows, Timothy; Lehman, Scott J.; Fifield, L Keith; De Deckker, Patrick


As the climate warmed at the end of the last glacial period, a rapid reversal in temperature, the Younger Dryas (YD) event, briefly returned much of the North Atlantic region to near full-glacial conditions. The event was associated with climate reversals in many other areas of the Northern Hemisphere and also with warming over and near Antarctica. However, the expression of the YD in the mid- to low latitudes of the Southern Hemisphere (and the southwest Pacific region in particular) is much...[Show more]

CollectionsANU Research Publications
Date published: 2007
Type: Journal article
Source: Science
DOI: 10.1126/science.1145873


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