2022
DOI: 10.1016/j.csr.2022.104764
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Tidal and wave modulation of rip current dynamics

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Cited by 4 publications
(3 citation statements)
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“…These factors induce variations in wave breaking intensity, thereby significantly altering the rip currents' morphology over time and space. This observation aligns with findings from other rip current studies [12,13,26]. Moreover, the velocity of rip currents in the arc-shaped beach area increases with wave height; at a wave height of 0.75 m, it approximates to 0.5 m/s, rising to 0.8 m/s at a significant wave height of 2.5 m. Generally, rip current velocities in this region exceed 0.5 m/s, corroborating findings from Dudkowska et al's research [42].…”
Section: Effect Of Significant Wave Height and Peak Period On Rip Cur...supporting
confidence: 94%
See 1 more Smart Citation
“…These factors induce variations in wave breaking intensity, thereby significantly altering the rip currents' morphology over time and space. This observation aligns with findings from other rip current studies [12,13,26]. Moreover, the velocity of rip currents in the arc-shaped beach area increases with wave height; at a wave height of 0.75 m, it approximates to 0.5 m/s, rising to 0.8 m/s at a significant wave height of 2.5 m. Generally, rip current velocities in this region exceed 0.5 m/s, corroborating findings from Dudkowska et al's research [42].…”
Section: Effect Of Significant Wave Height and Peak Period On Rip Cur...supporting
confidence: 94%
“…Their work provided insights into the factors contributing to the disruption of rip current persistence due to changes in wave angles. Zhang et al [13] conducted research on bay and sandbar channel topography, which is particularly susceptible to rip current hazards, and they explored variations in rip currents under the influence of tides and wave modulation. Hu et al [14] assessed rip current hazards on Hailing Island, China, considering factors such as water depth, tidal level and sediment dynamics.…”
Section: Introductionmentioning
confidence: 99%
“…There are many mechanisms for the generation of rip currents, including topographycontrolled rip currents generated by sandbars, sharp-angled beaches, and submerged reefs, wave-controlled rip currents generated by 3D waves, intersecting waves and wave clusters [2,7]. Most of the current studies on rip currents have focused on the measurement of depth-averaged velocities [8][9][10][11][12][13][14][15][16] or surface velocities [17][18][19][20][21]. Studies on the former mostly use Doppler acoustic point velocity (ADV) to measure velocities 1/3 of the way to the bottom of the water, and those on the latter use float tracer techniques to obtain the velocity vector field at the surface of the water (circulating flow field).…”
Section: Introductionmentioning
confidence: 99%