2017
DOI: 10.1061/(asce)hy.1943-7900.0001308
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Influence of Regular Surface Waves on the Propagation of Gravity Currents: Experimental and Numerical Modeling

Abstract: The propagation of gravity currents is analyzed in the presence of regular surface waves, 5 both experimentally and numerically, by using a full-depth lock-exchange configuration. Full- hydrodynamics of the density current is significantly affected by the presence of the wave 12 motion. In particular, the front shows a pulsating behavior, the shape of the front itself is

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Cited by 13 publications
(24 citation statements)
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References 47 publications
(71 reference statements)
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“…For example, Viviano and Musumeci et al [7][8][9] proposed simplified numerical models, which simulate turbulence by means of eddy viscosity formulation, to study the mechanism of waves. But when it comes to optimal design, computational fluid dynamics (CFD) turns out to be a better choice because it is more practical and it can overcome the limitations of experimental conditions [10][11][12][13][14][15][16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…For example, Viviano and Musumeci et al [7][8][9] proposed simplified numerical models, which simulate turbulence by means of eddy viscosity formulation, to study the mechanism of waves. But when it comes to optimal design, computational fluid dynamics (CFD) turns out to be a better choice because it is more practical and it can overcome the limitations of experimental conditions [10][11][12][13][14][15][16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…The interaction between gravity currents and oscillatory motion has been investigated only in a few works [8,[27][28][29]. Ng and Fu [27] studied numerically the spreading of viscous gravity currents propagating in intermediate and deep water depth conditions, observing that wave-induced streaming flow acting at the bottom is responsible for changes in the gravity current velocity speed.…”
Section: Introductionmentioning
confidence: 99%
“…They adopted a point release technique and observed the self-similar phase of the two fronts respectively propagating under regular surface waves in deep water condition. Musumeci et al [28] investigated the propagation of gravity currents under regular surface waves, modeling the phenomenon both experimentally and numerically. The gravity currents were modeled assuming low density difference and intermediate water depth conditions and adopted the lock-exchange problem for the generation of the gravity current.…”
Section: Introductionmentioning
confidence: 99%
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