The modification of turbulent thermal wind balance by non-traditional effects

DOI10.1017/jfm.2021.669zbMath1487.76105arXiv2103.08549OpenAlexW3136299318MaRDI QIDQ5152949

Matthew N. Crowe

Publication date: 28 September 2021

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

Full work available at URL: https://arxiv.org/abs/2103.08549

zbMATH Keywords

asymptotic solutiondispersionocean circulationturbulent mixinghorizontal buoyancy gradientnon-traditional rotating flow

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Asymptotic methods, singular perturbations applied to problems in fluid mechanics (76M45) Turbulent transport, mixing (76F25) Geophysical flows (76U60)

Cites Work

• Unnamed Item
• Unnamed Item
• A generalized mathematical model of geostrophic adjustment and frontogenesis: uniform potential vorticity
• Dynamical aspects of shallow sea fronts
• Inertial nonlinear equilibration of equatorial flows
• The evolution of a front in turbulent thermal wind balance. Part 1. Theory
• Submesoscale surface fronts and filaments: secondary circulation, buoyancy flux, and frontogenesis
• Large scale ocean models beyond the traditional approximation
• Laboratory experiments with tilted convective plumes on a centrifuge: a finite angle between the buoyancy force and the axis of rotation
• Near-inertial waves in the ocean: beyond the ‘traditional approximation’
• The evolution of a front in turbulent thermal wind balance. Part 2. Numerical simulations
• Flows in a rotating spherical shell: the equatorial case

This page was built for publication: The modification of turbulent thermal wind balance by non-traditional effects