Eddy formation in the bays of Kamchatka and fluxes to the open ocean

The Eastern Kamchatka Current (EKC) is the western boundary current of the North Pacific subpolar gyre. Southeast of the Kamchatka Peninsula lies a large anticyclonic eddy, the Kamchatka Eddy (KE). This eddy is quasi-stationary. More generally, the oceanic region east of the EKC contains many eddies...

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Bibliographic Details
Published in:Ocean Dynamics
Main Authors: L'Her, Alexandre, Reinert, Markus, Prants, Sergey, Carton, Xavier, Morvan, Mathieu
Format: Article in Journal/Newspaper
Language:English
Published: Springer Heidelberg 2021
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00816/92795/99457.pdf
https://doi.org/10.1007/s10236-021-01449-w
https://archimer.ifremer.fr/doc/00816/92795/