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Main Authors: Bobrovnikov, Oleksandr, Jones, Madison, Prasanna, Shriya, Smith, Josiah, Rybkin, Alexei, Pelinovsky, Efim
Format: Preprint
Published: 2025
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Online Access:https://arxiv.org/abs/2510.14177
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author Bobrovnikov, Oleksandr
Jones, Madison
Prasanna, Shriya
Smith, Josiah
Rybkin, Alexei
Pelinovsky, Efim
author_facet Bobrovnikov, Oleksandr
Jones, Madison
Prasanna, Shriya
Smith, Josiah
Rybkin, Alexei
Pelinovsky, Efim
contents We discuss the following inverse problem: given the run-up data of a tsunami wave, can we recover its initial shape? We study this problem within the framework of the non-linear shallow water equations, a model widely used to study tsunami propagation and inundation. Previously, it has been demonstrated that in the case of infinite sloping bathymetry, it is possible to recover the initial water displacement and velocity from shoreline readings \cite{Rybkin23,Rybkin24,Rybkin25}. We consider a finite sloping bathymerty. We show that it is possible to recover boundary conditions (water displacement and velocity) on a virtual buoy from the shoreline data. Further, we discuss stitching together the shallow water equations and the Boussinesq equation in a more complex piece-wise sloping bathymetry in order to recover the initial conditions, while incorporating the dispersion to our model.
format Preprint
id arxiv_https___arxiv_org_abs_2510_14177
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Reconstruction of the non-linear wave at a buoy from shoreline data and applications to the tsunami inverse problem for piece-wise sloping bathymetry
Bobrovnikov, Oleksandr
Jones, Madison
Prasanna, Shriya
Smith, Josiah
Rybkin, Alexei
Pelinovsky, Efim
Analysis of PDEs
We discuss the following inverse problem: given the run-up data of a tsunami wave, can we recover its initial shape? We study this problem within the framework of the non-linear shallow water equations, a model widely used to study tsunami propagation and inundation. Previously, it has been demonstrated that in the case of infinite sloping bathymetry, it is possible to recover the initial water displacement and velocity from shoreline readings \cite{Rybkin23,Rybkin24,Rybkin25}. We consider a finite sloping bathymerty. We show that it is possible to recover boundary conditions (water displacement and velocity) on a virtual buoy from the shoreline data. Further, we discuss stitching together the shallow water equations and the Boussinesq equation in a more complex piece-wise sloping bathymetry in order to recover the initial conditions, while incorporating the dispersion to our model.
title Reconstruction of the non-linear wave at a buoy from shoreline data and applications to the tsunami inverse problem for piece-wise sloping bathymetry
topic Analysis of PDEs
url https://arxiv.org/abs/2510.14177