Deglacial patterns of South Pacific overturning inferred from (231)Pa and (230)Th

The millennial-scale variability of the Atlantic Meridional Overturning Circulation (AMOC) is well documented for the last glacial termination and beyond. Despite its importance for the climate system, the evolution of the South Pacific overturning circulation (SPOC) is by far less well understood....

Descripción completa

Detalles Bibliográficos
Autores principales: Ronge, Thomas A., Lippold, Jörg, Geibert, Walter, Jaccard, Samuel L., Mieruch-Schnülle, Sebastian, Süfke, Finn, Tiedemann, Ralf
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8517020/
https://www.ncbi.nlm.nih.gov/pubmed/34650117
http://dx.doi.org/10.1038/s41598-021-00111-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8517020/
https://www.ncbi.nlm.nih.gov/pubmed/34650117
http://dx.doi.org/10.1038/s41598-021-00111-1

Ejemplares similares