A model of a frictionless double–diffusive gravity current on a horizontal surface

DOI10.1080/03091928508219270zbMath0585.76135OpenAlexW2139240243WikidataQ114640470 ScholiaQ114640470MaRDI QIDQ3712004

Trevor J. McDougall

Publication date: 1985

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091928508219270

zbMATH Keywords

boundary conditionsdensity currentdouble-diffusive convectionhorizontal surfacesteady solutionsconservation of momentumdouble-diffusive flux of buoyancydouble-diffusive gravity currententrainment of fluid

Mathematics Subject Classification ID

Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Diffusion and convection (76R99) Basic methods in fluid mechanics (76M99)

Cites Work

• Turbulent entrainment in stratified flows
• Dynamical aspects of shallow sea fronts

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