2001
DOI: 10.1238/physica.topical.097a00152
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Video Measurements of Fluid Velocities and Water Levels in Breaking Waves

Abstract: The cost-e¡ective measurement of the velocity £ow ¢elds in breaking water waves, using particle and correlation image velocimetry, is described. The £uid velocities are estimated by tracking the motion of neutrally buoyant particles and aeration structures. Results of the phase-ensemble-averaged velocity £ow ¢elds, time-averaged horizontal velocities and turbulence results are presented for laboratory waves breaking on a beach of slope 1:20 and for waves breaking over a submerged bar. A comparison of measureme… Show more

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Cited by 9 publications
(6 citation statements)
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“…This results in velocity estimates at intervals of $0.25 cm. More details of the experimental setup and the imaging and computational procedures are given by Govender et al [2002a].…”
Section: Experimental Conditions and Proceduresmentioning
confidence: 99%
“…This results in velocity estimates at intervals of $0.25 cm. More details of the experimental setup and the imaging and computational procedures are given by Govender et al [2002a].…”
Section: Experimental Conditions and Proceduresmentioning
confidence: 99%
“…The water levels and roller geometries were measured using the technique of video time stacks, and the velocity vector field of the wave was measured using DCIV. Details of the experimental setup, imaging, and computational procedures are given by Govender [1999] and Govender et al [2002]. However, a brief description will be provided here.…”
Section: Experimental Conditions and Proceduresmentioning
confidence: 99%
“…The video recording of the water levels was analyzed in order to extract a time stack (also referred to as a keogram by Govender et al [2002]) of the wave at each position along the wave flume. A time stack consists of a single vertical line of pixel intensity values extracted from a sequence of video frames and stacked side by side.…”
Section: Experimental Conditions and Proceduresmentioning
confidence: 99%
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“…την µηδενική αλληλεπίδραση µε το νερό, (β) τη δυνατότητα υψηλής συχνότητας καταγραφής και εποµένως την καταγραφή φαινοµένων γρήγορα εξελισσόµενων, όπως π.χ. της εξέλιξης θραυόµενου κύµατος(Govender et al, 2002), (γ) τη δυνατότητα καταγραφής της ελεύθερης επιφάνειας του νερού, τόσο χρονικής και χωρικής πληροφορίας σε αντίθεση µε τα σταθµήµετρα και (δ) αποτελεί µια σχετικά φθηνή εργαστηριακή λύση. 2% του ύψους του προσπίπτοντος κύµατος).…”
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