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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...
Autores principales: | Bendle, Jacob M., Palmer, Adrian P., Thorndycraft, Varyl R., Matthews, Ian P. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
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 |
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