2019
DOI: 10.1061/(asce)ww.1943-5460.0000525
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Three-Dimensional Hydrodynamics Associated with a Solitary Wave Traveling over an Alongshore Variable Shallow Shelf

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Cited by 5 publications
(4 citation statements)
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“…The HWRL EF assisted with LiDAR (Laser Scanner) to provide highly resolved bathymetric conditions for interpretation of hydrodynamic conditions and for numerical modeling. Researchers used optical measurement techniques (i.e., Particle Tracking and Particle Image Velocimetry-PTV and PIV) to capture the flow around the two islands (Lynett et al, 2019), and used novel techniques to measure the run-up around the island (Kaihatu et al, 2018;Han et al, 2020). These experiments generated a detailed data set for the calibration of an open source code based on the extended Boussinesq equations for interactive and real-time wave simulation (Lynett, 2016).…”
Section: Example Research Projects For Nheri 2016-2019mentioning
confidence: 99%
“…The HWRL EF assisted with LiDAR (Laser Scanner) to provide highly resolved bathymetric conditions for interpretation of hydrodynamic conditions and for numerical modeling. Researchers used optical measurement techniques (i.e., Particle Tracking and Particle Image Velocimetry-PTV and PIV) to capture the flow around the two islands (Lynett et al, 2019), and used novel techniques to measure the run-up around the island (Kaihatu et al, 2018;Han et al, 2020). These experiments generated a detailed data set for the calibration of an open source code based on the extended Boussinesq equations for interactive and real-time wave simulation (Lynett, 2016).…”
Section: Example Research Projects For Nheri 2016-2019mentioning
confidence: 99%
“…(1) p,q (t) are all zero and therefore B (1) is zero for all t. Therefore B (1) may be omitted from (8) as well. From the recurrence relations established in (8) and (10) we can determine all of the degrees of freedom. After the degrees of freedom are determined, the vertical velocity at the water surface is now calculated:…”
Section: Numerical Algorithmmentioning
confidence: 99%
“…We set a time step at ∆t = 0.16 and the spatial resolutions in the x− and y−directions are ∆x = 0.37 and ∆y = 0.10, respectively. M = 5 terms are included in the perturpation series, and the modes in the x− and y−directions are truncated to N x = 2 13 and N y = 2 10 , respectively. Figure 8 shows snapshots of the plan view of the water-surface displacement along with the corresponding bathymetry.…”
Section: Undular Bore Propagation Over a Continental Shelf With Periomentioning
confidence: 99%
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