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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Detalles Bibliográficos
Autores principales: Rainsley, Eleanor, Menviel, Laurie, Fogwill, Christopher J., Turney, Chris S. M., Hughes, Anna L. C., Rood, Dylan H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6085367/
https://www.ncbi.nlm.nih.gov/pubmed/30093676
http://dx.doi.org/10.1038/s41598-018-29226-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6085367/
https://www.ncbi.nlm.nih.gov/pubmed/30093676
http://dx.doi.org/10.1038/s41598-018-29226-8

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