Gaussian vortices centered at topographic extrema, combined with linear background flow, form quasi-stationary solutions for 2D topographic turbulence whose stability depends on background energy level.
2024 Two-dimensional turbulence above topography: Condensation transition and selection of minimum enstrophy solutions
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Final states of two-dimensional turbulence above large-scale topography: stationary vortex solutions and barotropic stability
Gaussian vortices centered at topographic extrema, combined with linear background flow, form quasi-stationary solutions for 2D topographic turbulence whose stability depends on background energy level.