Journal of the Atmospheric Sciences · 1985 · 89 citations · 0 references
EngineeringEarth SciencesOcean EngineeringComputational Fluid DynamicsFlow VisualizationFluid DynamicsBoundary Layer FlowBoundary LayersBoundary-layer TheoryInviscid FlowStratified FlowBlockingBoundary Conditions For Inviscid FlowBrunt-väisälä FrequencyStratified Flow SimulationTwo-dimensional Flow ModelingVelocity Profile In Boundary LayersWave Dynamics In Stratified FlowWave Propagation In Stratified Fluids
This paper describes some laboratory experiments with two-dimensional stratified flow over isolated topography, in which a novel configuration simulating a radiating upper boundary condition is employed. Several experimental tests show that the upper boundary is quite effective in absorbing energy. The properties of flow over five different obstacle shapes were obtained for a merge of values of the parameter Nh/U(h is obstacle height, N Brunt-Väisälä frequency and U towing velocity) from 0 to 4 (approximately). The main results of the study are 1) for 0 ≤ Nh/U ≤ 0.5 (±0.2), the flow is consistent with linear theory and Longs model; 2) for 0.5 ≲ Nh/U ≲ 2.0, upstream columnar disturbances are found which apparently propagate arbitrarily far upstream in an inviscid system. 3) overturning and rotors in the lee wave field occur for Nh/U ∼ 1.5; and 4) for Nh/U ∼ 2.0, blocked fluid is present upstream, and in some cases is also apparent downstream. This upstream blocking is due to the super-position of the propagating columnar disturbances; it will similarly extend arbitrarily far upstream given sufficient time.