Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1

Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1

The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic cooling, thought to have been initiated by North America fresh water runoff that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature re...

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Bibliographic Details
Main Authors:	Hogg, A, Ramsey, C, Staff, R, Southon, J, Turney, C, Palmer, J, Fenwick, P, Boswijk, G, Friedrich, M, Helle, G, Hughen, K, Jones, R, Kromer, B, Noronha, A, Reynard, L, Wacker, L
Format:	Journal article
Published:	Nature Publishing Group: Open Access Journals - Option C 2016

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