Abstract

This paper is concerned with the derivation of a well-balanced kinetic scheme to approximate a shallow flow model incorporating non-flat bottom topography and horizontal temperature gradients. The considered model equations, also called as Ripa system, are the non-homogeneous shallow water equations considering temperature gradients and non-uniform bottom topography. Due to the presence of temperature gradient terms, the steady state at rest is of primary interest from the physical point of view. However, capturing of this steady state is a challenging task for the applied numerical methods. The proposed well-balanced kinetic flux vector splitting (KFVS) scheme is non-oscillatory and second order accurate. The second order accuracy of the scheme is obtained by considering a MUSCL-type initial reconstruction and Runge-Kutta time stepping method. The scheme is applied to solve the model equations in one and two space dimensions. Several numerical case studies are carried out to validate the proposed numerical algorithm. The numerical results obtained are compared with those of staggered central NT scheme. The results obtained are also in good agreement with the recently published results in the literature, verifying the potential, efficiency, accuracy and robustness of the suggested numerical scheme.

Highlights

  • In the recent years, the study of hyperbolic systems with source terms has attracted much attention in the field of computational fluid dynamics (CFD) due to their wide rang physical and engineering applications

  • The present work deals with the numerical approximation of shallow water equations which have temperature fluctuations of prime interest [4]

  • A kinetic flux vector splitting scheme for shallow water equations dissipation in the FVS scheme is consistent with the Navier-Stokes viscous terms, the robustness of the KFVS schemes can be understood, i.e., the absence of numerical shock instability

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Summary

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Citation: Saleem MR, Ashraf W, Zia S, Ali I, Qamar S (2018) A kinetic flux vector splitting scheme for shallow water equations incorporating variable bottom topography and horizontal temperature gradients. PLoS ONE 13(5): e0197500. https://doi. org/10.1371/journal.pone.0197500 Data Availability Statement: All relevant data are within the paper and its Supporting Information files. Funding: The author(s) received no specific funding for this work. Competing interests: The authors have declared that no competing interests exist.

Introduction
Wi þ
Jacobian matrix
Numerical case studies
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Author Contributions
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