Greenland ice mass loss during the Younger Dryas driven by Atlantic Meridional Overturning Circulation feedbacks

Understanding feedbacks between the Greenland Ice Sheet (GrIS) and the Atlantic Meridional Overturning Circulation (AMOC) is crucial for reducing uncertainties over future sea level and ocean circulation change. Reconstructing past GrIS dynamics can extend the observational record and elucidate mech...

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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Rainsley, Eleanor, Menviel, Laurie, Fogwill, Christopher J., Turney, Chris S. M., Hughes, Anna L. C., Rood, Dylan H.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC6085367/
https://ncbi.nlm.nih.gov/pubmed/30093676
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-29226-8
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