Non-breaking and breaking solitary wave run-up

By Ying Li. Journal of Fluid Mechanics, 2000

203 citations recorded by the source corpus.

Subfields: Computational Mechanics, Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/c8dad36697b9a7dfb1df08af0a9813fdd67e0400

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Computational Mechanics

In Earth-Surface Processes

In Oceanography

Citations in the corpus

Analytical solutions for tsunami runup on a plane beach: single waves, N-waves and transient waves (2010, background): “…analytical and experimental work on the runup of breaking or non-breaking relatively short solitary waves such as reported by, e.g. Synolakis (1987), Briggs et al. (1995), Liu et al. (1995), Li & Raichlen (2001, 2002, 2003), Tonkin et al. (2003), Jensen et al. (2003) and Lynett et al. (2008).”
Estimation of wave run-up on smooth, impermeable slopes using the wave momentum flux parameter (2004, background): “(Li and Raichlen, 2002 noted this was nearly the case for solitary wave run-up.)”
Corrected Incompressible SPH method for accurate water-surface tracking in breaking waves (2008, methodology): “3 Quantitative comparison In order to further evaluate the accuracy of the proposed CISPH model, the simulation results of Cases II and IV are quantitatively compared to their corresponding experimental results (Li, 2000).”
High Order Weighted Essentially Nonoscillatory Schemes for Convection Dominated Problems (2009, background): “Nonbreaking and breaking solitary wave run-up is studied in [95].”
Depth‐integrated, non‐hydrostatic model for wave breaking and run‐up (2009, background): “Hall and Watts [29], Li and Raichlen [30], and Synolakis [31] conducted series of laboratory experiments for solitary wave transformation and run-up on a plane beach.”
On the solitary wave paradigm for tsunamis (2008, methodology): “Examples from the literature are numerous see, e.g., Goring [1978], Synolakis [1986, 1987], Synolakis and Deb [1988], Synolakis et al. [1988], Tadepalli and Synolakis [1994], Yeh et al. [1994], Briggs et al. [1995], Liu et al. [1995], Li [2000], Li and Raichlen [2001, 2002, 2003] , Tonkin et al. [2”
Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up (2010, methodology): “These experiments, which cover a wide range of non-breaking and breaking waves, have become an accepted test case for validation of runup models (Titov and Synolakis, 1995; Lynett et al., 2002; Li and Raichlen, 2002; Wei et al., 2006; and Roeber et al., 2010).”
Breaking Waves: Review of Characteristic Relationships (2013, methodology): “In conjunction to wave height, depth and slope parameters, the analysis of wave vortex parameters [Longuet-Higgins, 1982] and wave plunge distances [Smith and Kraus, 1991], through both empirical and numerical methods [Khayyer et al., 2008; Li, 2000; Vinje and Brevig, 1980; Cooker et al., 1990], hav”