Conventional versus pre-balanced forms of the shallow-water equations solved using finite-volume method

被引:7
|
作者
Lu, Xinhua [1 ]
Xie, Shengbai [2 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan 430072, Peoples R China
[2] Univ Delaware, Coll Ocean Earth & Environm, Newark, DE 19716 USA
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
FORCE; HLLC; Pre-balanced; Shallow-water equations; SLIC; Well-balanced; HYPERBOLIC CONSERVATION-LAWS; SEDIMENT TRANSPORT; NUMERICAL-MODEL; GRADIENT-METHOD; SOURCE TERMS; FLOW MODEL; SIMULATIONS; SURFACE; TOPOGRAPHY; SCHEME;
D O I
10.1016/j.ocemod.2016.04.002
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In the existing literature, various forms of governing equations have been proposed to solve the shallow-water equations (SWEs). Recently, attention has been dedicated to the so-called "pre-balanced" form, because finite-volume schemes that are designed on this basis satisfy the well-balanced property. In this study, we theoretically investigate the relationship between numerical schemes devised using approximate Riemann solvers in the framework of finite-volume methods for solving the conventional form of the SWEs and its "pre-balanced" variant. We find that the numerical schemes for solving these two forms of the SWEs turn out to be identical when some widely employed upwind or centered approximate Riemann solvers are adopted for the numerical flux evaluations, such as the HLL (Harten, Lax, and van Leer), HLLC (HLL solver with restoring the contact surface), FORCE (first-order centered), and SLIC (slope limited centered) schemes. Some numerical experiments are performed, which verify the validity of the result of our theoretical analysis. The theoretical and numerical results suggest that the "pre-balanced" SWEs variant is not superior to the conventional one for solving the SWEs using approximate Riemann solvers. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:113 / 120
页数:8
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