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...
Published in: | Ocean Dynamics |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer Heidelberg
2021
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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/ |