Arctic freshwater forcing of the Younger Dryas cold reversal

@article{Tarasov2005ArcticFF,
  title={Arctic freshwater forcing of the Younger Dryas cold reversal},
  author={Lev Tarasov and William Richard Peltier},
  journal={Nature},
  year={2005},
  volume={435},
  pages={662-665}
}
The last deglaciation was abruptly interrupted by a millennial-scale reversal to glacial conditions, the Younger Dryas cold event. This cold interval has been connected to a decrease in the rate of North Atlantic Deep Water formation and to a resulting weakening of the meridional overturning circulation owing to surface water freshening. In contrast, an earlier input of fresh water (meltwater pulse 1a), whose origin is disputed, apparently did not lead to a reduction of the meridional… 
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[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
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Using an Earth system model of intermediate complexity forced by continuously varying boundary conditions and a hypothetical profile of freshwater forcing, the model simulates Heinrich event 1 (H1),
The Younger Dryas and the Sea of Ancient Ice
Abstract We propose that prior to the Younger Dryas period, the Arctic Ocean supported extremely thick multi-year fast ice overlain by superimposed ice and firn. We re-introduce the historical term
A calibrated deglacial drainage chronology for the North American continent: evidence of an Arctic trigger for the Younger Dryas
Abstract We present a new deglacial meltwater drainage chronology for the North American ice-sheet complex using a 3D glacial systems model calibrated against a large set of paleo-proxies. Results
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