Lagrangian drift near a wavy boundary in a viscous oscillating flow
Lagrangian drift near a wavy boundary in a viscous oscillating flow
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Cambridge, UK: Cambridge University Press
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Language
English
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Cambridge, UK: Cambridge University Press
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The formation of sand ripples in oscillating flows is thought to be due to a steady streaming current which near the bottom is towards the crests. We present quantitative observations of this mean flow over self-formed and artificial ripples, by observing the displacement of a coloured filament after a number of oscillations in the simple situation...
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Lagrangian drift near a wavy boundary in a viscous oscillating flow
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TN_cdi_proquest_miscellaneous_34597969
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_34597969
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ISSN
0022-1120
E-ISSN
1469-7645
DOI
10.1017/S002211200900682X