Spinning ice floes reveal intensification of mesoscale eddies in the western Arctic Ocean

Under-ice eddies are prevalent in the major circulation system in the western Arctic Ocean, the Beaufort Gyre. Theoretical studies hypothesize that the eddy-driven overturning and the ice-ocean drag are crucial mechanisms of the gyre equilibration in response to atmospheric winds. However, due to se...

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Detalles Bibliográficos
Autores principales: Manucharyan, Georgy E., Lopez-Acosta, Rosalinda, Wilhelmus, Monica 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/PMC9054753/
https://www.ncbi.nlm.nih.gov/pubmed/35488008
http://dx.doi.org/10.1038/s41598-022-10712-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9054753/
https://www.ncbi.nlm.nih.gov/pubmed/35488008
http://dx.doi.org/10.1038/s41598-022-10712-z

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