Models of non-Boussinesq lock-exchange flow

被引:24
作者
Rotunno, R. [1 ]
Klemp, J. B. [1 ]
Bryan, G. H. [1 ]
Muraki, D. J. [2 ]
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[2] Simon Fraser Univ, Dept Math, Burnaby, BC V5A 1S6, Canada
基金
加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
gravity currents; shallow water flows; turbulence simulation; DIRECT NUMERICAL-SIMULATION; GRAVITY CURRENTS; FRONT SPEED; PART; DYNAMICS; CHANNEL; HEAD;
D O I
10.1017/jfm.2010.648
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Nearly all analytical models of lock-exchange flow are based on the shallow-water approximation. Since the latter approximation fails at the leading edges of the mutually intruding fluids of lock-exchange flow, solutions to the shallow-water equations can be obtained only through the specification of front conditions. In the present paper, analytic solutions to the shallow-water equations for non-Boussinesq lock-exchange flow are given for front conditions deriving from free-boundary arguments. Analytic solutions are also derived for other proposed front conditions - conditions which appear to the shallow-water system as forced boundary conditions. Both solutions to the shallow-water equations are compared with the numerical solutions of the Navier-Stokes equations and a mixture of successes and failures is recorded. The apparent success of some aspects of the forced solutions of the shallow-water equations, together with the fact that in a real fluid the density interface is a free boundary, shows the need for an improved theory of lock-exchange flow taking into account non-hydrostatic effects for density interfaces intersecting rigid boundaries.
引用
收藏
页码:1 / 26
页数:26
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