Glacier fluctuations in the northern Patagonian Andes (44°S) imply wind-modulated interhemispheric in-phase climate shifts during Termination 1

The Last Glacial Termination (T1) featured major changes in global circulation systems that led to a shift from glacial to interglacial climate. While polar ice cores attest to an antiphased thermal pattern at millennial timescales, recent well-dated moraine records from both hemispheres suggest in-...

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Detalles Bibliográficos
Autores principales: Soteres, Rodrigo L., Sagredo, Esteban A., Kaplan, Michael R., Martini, Mateo A., Moreno, Patricio I., Reynhout, Scott A., Schwartz, Roseanne, Schaefer, Joerg M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9237032/
https://www.ncbi.nlm.nih.gov/pubmed/35761034
http://dx.doi.org/10.1038/s41598-022-14921-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9237032/
https://www.ncbi.nlm.nih.gov/pubmed/35761034
http://dx.doi.org/10.1038/s41598-022-14921-4

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