Tsunami run-up and draw-down on a plane beach

By George F. Carrier, T. Wu, H. Yeh. Journal of Fluid Mechanics, 2003

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Estimation of wave run-up on smooth, impermeable slopes using the wave momentum flux parameter (2004, methodology): “Carrier et al. (2003) crafted an analytical formulation for tsumani run-up, and they noted the location and direction of maximum wave momentum flux for the cases of initial positive and negative wave forms.”
Analytical solutions for tsunami runup on a plane beach: single waves, N-waves and transient waves (2010, background): “Runup solution for N-waves The runup of leading depression waves (i.e. waves with a small negative leading wave followed by a higher positive one) has been studied by, e.g. Pelinovsky & Mazova (1992), Tadepalli & Synolakis (1994, 1996), Carrier et al. (2003) and Kânoğlu (2004).”
Tsunami science before and beyond Boxing Day 2004 (2006, unknown): “The Carrier et al. (2003) solution includes integrals with singularities and ad hoc linearizations of the transformation, issues addressed shortly thereafter by Kanoglu (2004).”
Tsunami-like solitary waves impinging and overtopping an impermeable seawall: Experiment and RANS modeling (2010, background): “Particularly, solitary waves interacting with coastal objects have garnered considerable attention in terms of wave run-up on a uniform slope (e.g. Lin et al., 1999; Carrier et al., 2003; Li and Raichlen, 2003; Hsiao et al., 2008; Chang et al., 2009), disintegration and transmission properties of wa”