Meridional dynamics of grounded abyssal water masses on a sloping bottom in a mid-latitude -plane

DOI10.1017/JFM.2018.17zbMath1419.86015OpenAlexW2794162861MaRDI QIDQ5227037

Gordon E. Swaters

Publication date: 5 August 2019

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://semanticscholar.org/paper/179f6b70d011e7d1d8caa1aaf7f4d8f0bd8f0a93

zbMATH Keywords

ocean circulationgeophysical and geological flows

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Stability and instability of geophysical and astrophysical flows (76E20) PDEs in connection with geophysics (35Q86)

Cites Work

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• Mixed bottom-friction–Kelvin–Helmholtz destabilization of source-driven abyssal overflows in the ocean
• Baroclinic characteristics of frictionally destabilized abyssal overflows
• Hamiltonian Structure and a Variational Principle for Grounded Abyssal Flow on a Sloping Bottom in a Mid‐Latitude β‐Plane
• On the baroclinic instability of cold-core coupled density fronts on a sloping continental shelf
• Flow of grounded abyssal ocean currents along zonally-varying topography on a rotating sphere
• Cross-equatorial flow of grounded abyssal ocean currents
• Internal dissipative boundary layers in the cross-equatorial flow of a grounded deep western boundary current

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