Mixed bottom-friction–Kelvin–Helmholtz destabilization of source-driven abyssal overflows in the ocean
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Publication:3184095
DOI10.1017/S0022112008005673zbMath1171.76379OpenAlexW2057089679MaRDI QIDQ3184095
Publication date: 13 October 2009
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112008005673
Hydrology, hydrography, oceanography (86A05) Stability and instability of geophysical and astrophysical flows (76E20)
Related Items (4)
Ekman destabilization of inertially stable baroclinic abyssal flow on a sloping bottom ⋮ Turbulent hydraulic jumps in a stratified shear flow ⋮ Meridional dynamics of grounded abyssal water masses on a sloping bottom in a mid-latitude -plane ⋮ Flow of grounded abyssal ocean currents along zonally-varying topography on a rotating sphere
Cites Work
- On the frictional destabilization of abyssal overflows dynamically coupled to internal gravity waves
- Baroclinic characteristics of frictionally destabilized abyssal overflows
- Dynamics of roll waves
- Ageostrophic instabilities in a horizontally uniform baroclinic flow along a slope
- On the baroclinic instability of cold-core coupled density fronts on a sloping continental shelf
- Dynamics of ventilated coherent cold eddies on a sloping bottom
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