论文标题
洪水模型中的摩擦脱钩和旋转不变性的损失
Friction decoupling and loss of rotational invariance in flooding models
论文作者
论文摘要
摩擦解耦,即摩擦矢量成分的计算,可以单独使用相应的速度成分,这在SWE简化的交错网格模型(零内政和局部惯性近似)中很常见,由于程序简单性以及对随之而来的计算的加速。在本文中,从理论和数值的角度研究了摩擦解耦的效果。首先,已经发现,摩擦矢量解耦会导致计算的摩擦力减少和摩擦力向量的旋转。其次,已经证明,解耦摩擦模型缺乏旋转不变性,即模型结果取决于参考框架的比对。这些理论结果已通过数值实验证实。在此基础上,很明显,摩擦向量的解耦会导致相应的数学和数值模型的可信度重大丧失。尽管脱钩摩擦计算的加速速度适中,但在每种情况下都应优选经典的耦合摩擦模型。
Friction decoupling, i.e. the computation of friction vector components making separate use of the corresponding velocity components, is common in staggered grid models of the SWE simplifications (Zero-Inertia and Local Inertia Approximation), due to the programming simplicity and to the consequent calculations speed-up. In the present paper, the effect of friction decoupling has been studied from the theoretical and numerical point of view. First, it has been found that friction vector decoupling causes the reduction of the computed friction force and the rotation of the friction force vector. Second, it has been demonstrated that decoupled-friction models lack of rotational invariance, i.e. model results depend on the alignment of the reference framework. These theoretical results have been confirmed by means of numerical experiments. On this basis, it is evident that the decoupling of the friction vector causes a major loss of credibility of the corresponding mathematical and numerical models. Despite the modest speed-up of decoupled-friction computations, classic coupled-friction models should be preferred in every case.