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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Detalles Bibliográficos
Autores principales: Hogg, Alan, Southon, John, Turney, Chris, Palmer, Jonathan, Bronk Ramsey, Christopher, Fenwick, Pavla, Boswijk, Gretel, Friedrich, Michael, Helle, Gerhard, Hughen, Konrad, Jones, Richard, Kromer, Bernd, Noronha, Alexandra, Reynard, Linda, Staff, Richard, Wacker, Lukas
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4872135/
https://www.ncbi.nlm.nih.gov/pubmed/27194601
http://dx.doi.org/10.1038/srep25902

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