Abstract
Eddy or low frequency (periods greater than a day) kinetic energy per unit mass (KE) in the western North Atlantic is observed to increase approaching the Gulf Stream system along 55W longitude from the interior of the subtropical gyre, by a factor of 30 in the thermocline and by over two orders of magnitude at 4000 m depth....
Recommended Citation
Schmitz, William J.. 1978. "Observations of the vertical distribution of low frequency kinetic energy in the western North Atlantic." Journal of Marine Research 36, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1431
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