1983
DOI: 10.1007/bf00282269
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Visualization of particle displacement and flow in stratified salt water

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1986
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Cited by 9 publications
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“…The vortex dipole thickness H was measured using a simple technique proposed by Gartner (1983). Observations demonstrate that after the dipole has been formed (t > to) its thickness R does not vary with time, hence f (~~, T * ) = const.…”
Section: Vortex Dipole Characteristicsmentioning
confidence: 99%
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“…The vortex dipole thickness H was measured using a simple technique proposed by Gartner (1983). Observations demonstrate that after the dipole has been formed (t > to) its thickness R does not vary with time, hence f (~~, T * ) = const.…”
Section: Vortex Dipole Characteristicsmentioning
confidence: 99%
“…In our previous experiments(Voropayev & Filippov 1985) the thickness H of the front region was not measured. Using the simple technique proposed byGartner (1983) we have made these measurements and the results are shown in figure 12 in a non-dimensional form (the values of ro for different z a n d J were calculated using the relation (2.12) and the graph infigure 11).Introducing the Reynolds number of the front regionRe = 2RO/v = apAJ (2.20), (2.22) we have a simple estimate for the 'age' of the flow : t = Z/20. (2.24)…”
mentioning
confidence: 99%