Systematic forcing of large-scale geophysical flows by eddy-topography interaction

DOI10.1017/S0022112087002970zbMath0634.76112OpenAlexW4365787291WikidataQ114654722 ScholiaQ114654722MaRDI QIDQ3773634

Greg Holloway

Publication date: 1987

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

Full work available at URL: https://doi.org/10.1017/s0022112087002970

zbMATH Keywords

interaction of eddieslarge-scale mean flowslarge-scale wave propagationoceanic Antarctic Circumpolar Currentvariations in topography

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Reaction effects in flows (76V05) Basic methods in fluid mechanics (76M99)

Related Items (11)

A generalized theory of flow forcing by rough topography ⋮ Spin-down of a baroclinic vortex by irregular small-scale topography ⋮ Spin-down of a barotropic vortex by irregular small-scale topography ⋮ Rectified flow of a rotating fluid along a vertical sidewall ⋮ Low-dimensional reduced-order models for statistical response and uncertainty quantification: barotropic turbulence with topography ⋮ The sandpaper theory of flow–topography interaction for homogeneous shallow-water systems ⋮ Passive scalar transport in β-plane turbulence ⋮ Moments of probable seas: statistical dynamics of Planet Ocean ⋮ Correlation-based flow decomposition and statistical analysis of the eddy forcing ⋮ Beta-plane turbulence above monoscale topography ⋮ Flow–topography interactions in shallow-water turbulence

Cites Work

• The structure of isotropic turbulence at very high Reynolds numbers
• H theorems in statistical fluid dynamics
• Evolution of high Reynolds number two-dimensional turbulence
• The equilibrium statistical mechanics of simple quasi-geostrophic models
• Stochastic closure for nonlinear Rossby waves
• Analytical theories of turbulence
• An almost-Markovian Galilean-invariant turbulence model
• Numerical Simulation of Incompressible Flows Within Simple Boundaries. I. Galerkin (Spectral) Representations

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