Modeling swash‐zone hydrodynamics and shear stresses on planar slopes using Reynolds‐Averaged Navier–Stokes equations. Issue 2 (11th February 2013)

• Record Type: Journal Article
• Authors: Torres‐Freyermuth, Alec; Puleo, Jack A.; Pokrajac, Dubravka
• Is Part Of: Journal of geophysical research. Volume 118:Issue 2(2013:Feb.)
• Page Start: 1019
• Page End: 1033
• Publication Date: 2013-02-11
• Subjects: swash zone; Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/jgrc.20074
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract: [1] A numerical model solving the Reynolds‐Averaged Navier–Stokes equations, with a volume of fluid‐tracking scheme and turbulence closure, is employed for estimating hydrodynamics in the swash zone. Model results for run‐up distance, water depth, and near‐bed velocity are highly correlated ( r 2 > 0.97) with ensemble‐averaged dam‐break‐driven swash data. Moreover, modeled bed shear stresses are within 20% of estimates derived from measured velocity profiles. Dam‐break‐driven swash simulations are conducted to determine the effect of foreshore characteristics (bed roughness and foreshore slope) on bore‐induced swash‐zone hydrodynamics and bed shear stresses. Numerical results revealed that the boundary layer vanishes during flow reversal, grows during the backwash, and becomes depth limited at the end of the swash cycle. In general, the uprush experiences larger shear stresses but for a shorter duration than the backwash. Some variability in this pattern is observed depending on the bed roughness, foreshore slope, and cross‐slope location in the swash zone, implying that large spatial gradients in shear stresses can occur on the foreshore. The mean tangential force per unit area supplied to the bed is offshore directed for the simulated cases, with the exception of the mild‐slope (1:25) cases, owing to the skewed nature of swash flows. The temporal evolution of the momentum balance inside the swash zone shows an important contribution to the total force from turbulence and advection at the early/final stage of the swash cycle, whereas the local acceleration does not appear to be a significant contribution. Key Points: VOF RANS model validation with high‐resolution laboratory swash data Model application to study spatiotemporal variability of bed shear stresses