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- W2005707830 abstract "A linear model with cabbeling dynamics is developed for a nonrotating, unstratified ocean and applied to observations of three medium- to large-scale oceanic thermohaline (density balanced) fronts. The ability of the predicted cabbeling sinking and surface convergence rates to maintain a steady front against diffusion depends critically on the assumed values of horizontal and vertical eddy viscosities. There is good theoretical evidence for the existence of small-scale (1 km), weak (surface currents 0.1 cm s−1) cabbeling fronts; however, the intensity and stability of such fronts will depend critically on the scale dependent behavior of dissipation processes." @default.
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- W2005707830 date "1978-01-01" @default.
- W2005707830 modified "2023-10-18" @default.
- W2005707830 title "Cabbeling at thermohaline fronts" @default.
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- W2005707830 doi "https://doi.org/10.1029/jc083ic12p06173" @default.
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