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Two-Layer Viscous Shallow-Water Equations and Conservation Laws

机译:两层粘性浅水方程和守恒律

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References(12) Cited-By(1) In our previous papers, the two-layer viscous shallow-water equations were derived from the three-dimensional Navier-Stokes equations under the hydrostatic assumption. Also, it was noted that the combination of upper and lower equations in the two-layer model produces the classical one-layer equations if the density of each layer is the same. Then, the two-layer equations were approximated by a finite element method which followed our numerical scheme established for the one-layer model in 1978. Also, it was numerically demonstrated that the interfacial instability generated when the densities are the same can be eliminated by providing a sufficient density difference. In this paper, we newly show that conservation laws are still valid in the two-layer model. Also, we show results of a new physical experiment for the interfacial instability.
机译:参考文献(12)Cited-By(1)在我们以前的论文中,两层粘性浅水方程是在静水力假设下从三维Navier-Stokes方程导出的。同样,要注意的是,如果每一层的密度相同,则两层模型中上下方程的组合会产生经典的一层方程。然后,采用有限元方法对两层方程进行近似,该方法遵循我们在1978年为单层模型建立的数值方案。而且,数值证明了可以消除密度相同时产生的界面不稳定性。提供足够的密度差。在本文中,我们新证明了守恒律在两层模型中仍然有效。此外,我们显示了界面不稳定性新物理实验的结果。

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