Routes of the Upper Branch of the Atlantic Meridional Overturning Circulation according to an Ocean State Estimate

The origins of the upper branch of the Atlantic meridional overturning circulation (AMOC) are traced with backward‐in‐time Lagrangian trajectories, quantifying the partition of volume transport between different routes of entry from the Indo‐Pacific into the Atlantic. Particles are advected by the v...

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Detalles Bibliográficos
Autores principales: Rousselet, Louise, Cessi, Paola, Forget, Gael
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2020
Materias:
Research Letters
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7757194/
https://www.ncbi.nlm.nih.gov/pubmed/33380755
http://dx.doi.org/10.1029/2020GL089137

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7757194/
https://www.ncbi.nlm.nih.gov/pubmed/33380755
http://dx.doi.org/10.1029/2020GL089137

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