Abstract

ABSTRACT The one-dimensional flow routing inertial model, formulated as an explicit solution, has advantages over other explicit models used in hydrological models that simplify the Saint-Venant equations. The main advantage is a simple formulation with good results. However, the inertial model is restricted to a small time step to avoid numerical instability. This paper proposes six numerical schemes that modify the one-dimensional inertial model in order to increase the numerical stability of the solution. The proposed numerical schemes were compared to the original scheme in four situations of river’s slope (normal, low, high and very high) and in two situations where the river is subject to downstream effects (dam backwater and tides). The results are discussed in terms of stability, peak flow, processing time, volume conservation error and RMSE (Root Mean Square Error). In general, the schemes showed improvement relative to each type of application. In particular, the numerical scheme here called Prog Q(k+1)xQ(k+1) stood out presenting advantages with greater numerical stability in relation to the original scheme. However, this scheme was not successful in the tide simulation situation. In addition, it was observed that the inclusion of the hydraulic radius calculation without simplification in the numerical schemes improved the results without increasing the computational time.

Highlights

  • River’s flow and the propagation of flood waves can be represented by hydrodynamic models that solve numerically the Saint-Venant equations

  • The inclusion of the hydraulic radius calculation in numerical schemes reduced the RMSE by 20% in the original scheme and by 30% in the progressive derivative (Prog) Q(k+1)xQ(k+1) scheme

  • This paper compared the performance of new numerical schemes with inertial approximation of the Saint-Venant equations

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Summary

Introduction

River’s flow and the propagation of flood waves can be represented by hydrodynamic models that solve numerically the Saint-Venant equations. These are formed by the continuity equation (Equation 1), which represents the mass conservation, and by the dynamic equation (Equation 2), which represents the forces acting on the flow (CUNGE; HOLLY; VERWEY, 1980; TUCCI, 2005). The two equations are presented considering a one-dimensional flow.

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