Experiments on 2–D submerged vertical jets with progressive water surface waves

The effect of progressive water surface waves on two-dimensional vertical impinging jets is studied experimentally. The submerged turbulent jets were generated by discharging water through a slot orifice into a water ambient. The velocity profiles across and along the jet center plane at x = 0 were measured with a laser Doppler velocimeter (LDV) for cases with and without surface waves. The experimental results show that for the case with waves: (1) the mean velocity profile of jet remains Gaussian and self-similar in the zone of established flow (ZEF); (2) the waves enhance the jet mixing by approximately 30%, as by comparing the spreading constant of oc=l .6 for jet with waves to that of α=l .2 for jet without waves; and (3) the surface waves will cause the jet maximum centerline to deflect from the center plane of x=0.

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Publication Details

Published
2026-02-12
DOI
https://doi.org/10.1201/9781003761877_ch22
Citations
1
Primary Topic
Tropical and Extratropical Cyclones Research
Type
article
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article

Experiments on 2–D submerged vertical jets with progressive water surface waves

J. S. Kuang, C. C. Hsu
1 citations
Tropical and Extratropical Cyclones Research
article

Experiments on 2–D submerged vertical jets with progressive water surface waves

J. S. Kuang, C. C. Hsu
article en
1 citations

Abstract

The effect of progressive water surface waves on two-dimensional vertical impinging jets is studied experimentally. The submerged turbulent jets were generated by discharging water through a slot orifice into a water ambient. The velocity profiles across and along the jet center plane at x = 0 were measured with a laser Doppler velocimeter (LDV) for cases with and without surface waves. The experimental results show that for the case with waves: (1) the mean velocity profile of jet remains Gaussian and self-similar in the zone of established flow (ZEF); (2) the waves enhance the jet mixing by approximately 30%, as by comparing the spreading constant of oc=l .6 for jet with waves to that of α=l .2 for jet without waves; and (3) the surface waves will cause the jet maximum centerline to deflect from the center plane of x=0.

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Tropical and Extratropical Cyclones Research
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