The Younger Dryas: From whence the fresh water?


[1] Oxygen isotopic records of meltwater outflow and records of sea level change do not support the idea that fresh waters derived solely from the melting of Northern Hemisphere ice sheets was likely to have stabilized the upper layers of the North Atlantic Ocean and prevented deep convection during the Younger Dryas. Yet there are paleoceanographic… (More)


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@inproceedings{Moore2005TheYD, title={The Younger Dryas: From whence the fresh water?}, author={Timothy C. Moore}, year={2005} }