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- W2077895715 abstract "[1] Upper-ocean eddies are commonly observed from remote sensing, but submerged eddies are more difficult to detect. During July 2004, a 21-day hydrographic survey in the southern region of the California Current was carried out to investigate the mesoscale variability. We observed for the first time a subsurface anticyclonic eddy off northern Baja California with the same water mass characteristics as the California Undercurrent. The core of the eddy was quasi-circular with radii of 35 km and thickness of 250 m. The maximum swirl velocity was ∼3 cms−1. The water mass of the core of the eddy was characterized by potential temperature of 11°C, salinity of 34.5, and dissolved oxygen of 1.4 mll−1. The eddy propagated westward. The subsurface warm-eddy could transport relatively saline water into the North Pacific subtropical gyre." @default.
- W2077895715 created "2016-06-24" @default.
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- W2077895715 date "2007-03-30" @default.
- W2077895715 modified "2023-10-12" @default.
- W2077895715 title "A subsurface warm-eddy off northern Baja California in July 2004" @default.
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- W2077895715 doi "https://doi.org/10.1029/2006gl028851" @default.
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