The transition from inertia- to bottom-drag-dominated motion of turbulent gravity currents
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Publication:2774085
DOI10.1017/S0022112001006292zbMath1015.76035WikidataQ109767520 ScholiaQ109767520MaRDI QIDQ2774085
Andrew J. Hogg, Andrew W. Woods
Publication date: 5 August 2003
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
similarity solutionsperturbation seriesdragparticle sedimentationboundary shear stressChézy modelformation of discontinuityparticle-driven currentsturbulent gravity currents
Related Items (6)
Experimental and numerical simulation of three-dimensional gravity currents on smooth and rough bottom ⋮ Sustained gravity currents in a channel ⋮ Gravity currents from a line source in an ambient flow ⋮ Collapse of a neutrally buoyant suspension column: from Newtonian to apparent non-Newtonian flow regimes ⋮ Steady and unsteady fluidised granular flows down slopes ⋮ Entraining gravity currents
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