Turbulence, Horizontal Convection, and the Ocean’s Meridional Overturning Circulation
From MaRDI portal
Publication:5272902
DOI10.1007/978-3-319-39092-5_2zbMath1366.86013OpenAlexW2557157618WikidataQ60551408 ScholiaQ60551408MaRDI QIDQ5272902
Publication date: 5 July 2017
Published in: Mathematical Paradigms of Climate Science (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/978-3-319-39092-5_2
turbulenceenergy dissipationhorizontal convectionKolmogorov's 1941 theorymeridional overturning circulation
Hydrology, hydrography, oceanography (86A05) Meteorology and atmospheric physics (86A10) Convective turbulence (76F35)
Cites Work
- Unnamed Item
- Unnamed Item
- Stressed horizontal convection
- ON THE SMALLNESS OF SINKING REGIONS IN THE OCEAN
- On the energetics of stratified turbulent mixing, irreversible thermodynamics, Boussinesq models and the ocean heat engine controversy
- Energy dissipation in a shear layer with suction
- Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks
- Shear dispersion
- An Introduction to Fluid Dynamics
- Atmospheric and Oceanic Fluid Dynamics
- Bounds on horizontal convection
- Horizontal convection is non-turbulent
- Available potential energy and buoyancy variance in horizontal convection
- A theoretical model for horizontal convection at high Rayleigh number
- Weather Prediction by Numerical Process
- Energetics of horizontal convection
- Rotating horizontal convection
- Horizontal Convection
- V<scp>ERTICAL</scp> M<scp>IXING</scp>, E<scp>NERGY</scp>, <scp>AND THE</scp> G<scp>ENERAL</scp> C<scp>IRCULATION OF THE</scp> O<scp>CEANS</scp>
This page was built for publication: Turbulence, Horizontal Convection, and the Ocean’s Meridional Overturning Circulation