Decadal changes in Atlantic overturning due to the excessive 1990s Labrador Sea convection

Changes in the Atlantic Meridional Overturning Circulation (AMOC) represent a crucial component of Northern Hemisphere climate variability. In modelling studies decadal overturning variability has been attributed to the intensity of deep winter convection in the Labrador Sea. This linkage is challen...

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Detalles Bibliográficos
Autores principales: Böning, C. W., Wagner, P., Handmann, P., Schwarzkopf, F. U., Getzlaff, K., Biastoch, A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10397207/
https://www.ncbi.nlm.nih.gov/pubmed/37532713
http://dx.doi.org/10.1038/s41467-023-40323-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10397207/
https://www.ncbi.nlm.nih.gov/pubmed/37532713
http://dx.doi.org/10.1038/s41467-023-40323-9

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