A two-layer non-hydrostatic landslide model for tsunami generation on irregular bathymetry. 1. Theoretical basis. (March 2021)

• Record Type: Journal Article
• Authors: Zhang, Cheng; Kirby, James T.; Shi, Fengyan; Ma, Gangfeng; Grilli, Stephan T.
• Is Part Of: Ocean modelling. Volume 159(2021)
• Publication Date: 2021-03
• Subjects: Submarine landslide -- Two-layer non-hydrostatic model -- Tsunami propagation -- Rheology closures; Oceanography -- Periodicals; Océanographie -- Périodiques; Oceanography; Periodicals; 551.46
• DOI: 10.1016/j.ocemod.2020.101749
• Languages: English
• ISSNs: 1463-5003

Abstract

Abstract: We describe a two-layer, coupled model for landslide motion over irregular bathymetry and resulting water column motion and tsunami generation. The three-dimensional non-hydrostatic wave model NHWAVE (Ma et al., 2012) is applied as the upper-layer model to simulate landslide-generated tsunami waves. Here, we focus on the derivation of governing equations for the lower-layer model, where the landslide is described as either a viscous mud flow or a saturated granular debris flow. The governing equations are depth-integrated in a Cartesian coordinate system referenced to the still water surface. Vertical acceleration of the slide is taken into account by including non-hydrostatic pressure effects within the slide. The model is validated in comparison to analytic results of Mangeney et al. (2000) and the slope-oriented numerical approach of Ma et al. (2015). The numerical approach and further examples are described in the companion paper Zhang et al. (2021). Highlights: A two-layer model is developed for investigating tsunamis generated by landslides. The low-layer landslide model is developed on a standard Cartesian coordinate. Non-hydrostatic pressure effects are accounted for the slide vertical acceleration. The landslide is formulated as a mud flow or a granular flow. New algorithms of rheology closures are introduced.