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Coupling superposed 1D and 2D shallow-water models: Source terms in finite volume schemes

机译:耦合叠加的1D和2D浅水模型:有限体积方案中的源项

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We study the superposition of 1D and 2D shallow-water equations with non-flat topographies, in the context of river-flood modeling. Since we superpose both models in the bi-dimensional areas, we focus on the definition of the coupling term required in the 1D equations. Using explicit finite volume schemes, we propose a definition of the discrete coupling term leading to schemes globally well-balanced (the global scheme preserves water at rest whatever if overflowing or not). For both equations (1D and 2D), we can consider independent finite volume schemes based on well-balanced Roe, HLL, Rusanov or other scheme, then the resulting global scheme remains well-balanced. We perform a few numerical tests showing on the one hand the well-balanced property of the resulting global numerical model, on the other hand the accuracy and robustness of our superposition approach. Therefore, the definition of the coupling term we present allows to superpose a local 2D model over a 1D main channel model, with non-flat topographies and mix incoming-outgoing lateral fluxes, using independent grids and finite volume solvers.
机译:在河流洪水建模的背景下,我们研究了一维和二维浅水方程与非平坦地形的叠加。由于我们将两个模型都叠加在二维区域中,因此我们将重点放在一维方程中所需的耦合项的定义上。通过使用显式有限体积方案,我们提出了离散耦合项的定义,从而导致了方案在全局上达到了良好的平衡(全局方案无论是否有溢水,均能保持静止的水)。对于这两个方程(1D和2D),我们可以考虑基于均衡Roe,HLL,Rusanov或其他方案的独立有限体积方案,然后所得的全局方案仍保持均衡。我们进行了一些数值测试,一方面表明了所得全局数值模型的均衡特性,另一方面表明了我们叠加方法的准确性和鲁棒性。因此,我们现在给出的耦合项的定义允许使用非平面地形将局部2D模型叠加到1D主通道模型上,并使用独立的网格和有限体积求解器来混合传入的输出横向通量。

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