Journal
PROCEEDINGS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES
Volume 457, Issue 2016, Pages 2827-2830Publisher
ROYAL SOC
DOI: 10.1098/rspa.2001.0802
Keywords
stratified flow; topography; mixing; entrainment
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Essential mechanisms identified in the authors' observations of flow establishment over topography are restated, with emphasis on those which are at variance with numerical simulations. Specifically, small-scale instabilities were observed to lead to upwards transport of fluid from the primary flow so as to form a nearly stationary intermediate layer, and boundary-layer separation significantly delays establishment of the downslope flow. Simulations that force the streamlines to follow the topography generate a large-amplitude breaking wave, which we did not observe. Our observations show that small-scale instability and separation act in concert to determine the time-dependent evolution of the stratified flow response.
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