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- W2084973088 abstract "High-speed currents within the Arctic Ocean pycnocline are associated with small baroclinic eddies, most of which appear to be anticyclonic. A typical eddy has a central core with a radius of about 6 km, which is in solid-body rotation. This core is surrounded by a region of large vorticity gradient. At radii greater than about 8 km the motion is nearly irrotational, although the eddy noticeably influences the velocity field out to about 15 km from the center. Such eddies are apparent in 13−12 of the available current records and hence represent a fairly common feature. T-S correlations in the eddies differ from those in the ambient waters, implying that the eddies are not locally generated." @default.
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- W2084973088 date "1974-09-01" @default.
- W2084973088 modified "2023-10-15" @default.
- W2084973088 title "Baroclinic eddies in the Arctic Ocean" @default.
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- W2084973088 doi "https://doi.org/10.1016/0011-7471(74)90078-3" @default.
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