Phased Patagonian Ice Sheet response to Southern Hemisphere atmospheric and oceanic warming between 18 and 17 ka

The onset of deglaciation in the Southern Hemisphere mid-latitudes has been attributed to the southward transmission of climate anomalies in response to slow-down of Atlantic meridional overturning circulation (AMOC) during Heinrich Stadial 1 (HS-1; 18–14.6 ka). However, inferences on the response o...

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Detalles Bibliográficos
Autores principales: Bendle, Jacob M., Palmer, Adrian P., Thorndycraft, Varyl R., Matthews, Ian P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6411896/
https://www.ncbi.nlm.nih.gov/pubmed/30858415
http://dx.doi.org/10.1038/s41598-019-39750-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6411896/
https://www.ncbi.nlm.nih.gov/pubmed/30858415
http://dx.doi.org/10.1038/s41598-019-39750-w

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