High-order interpolation schemes for shear instability simulations
Author(s) -
Shooka Karimpour,
Vincent H. Chu
Publication year - 2015
Publication title -
international journal of numerical methods for heat andamp fluid flow
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.85
H-Index - 52
eISSN - 1758-6585
pISSN - 0961-5539
DOI - 10.1108/hff-07-2014-0235
Subject(s) - froude number , instability , interpolation (computer graphics) , shear (geology) , grid , mechanics , convective instability , mathematics , geology , classical mechanics , physics , geometry , flow (mathematics) , petrology , motion (physics)
Purpose: The purpose of this paper is to evaluate the performance of a numerical method for the solution to shallow-water equations on a staggered grid, in simulations for shear instabilities at two convective Froude numbers.Design/methodology/approach: The simulations start from a small perturbation to a base flow with a hyperbolic-tangent velocity profile. The subsequent development of the shear instabilities is studied from the simulations using a number of flux-limiting schemes, including the second-order MINMOD, the third-order ULTRA-QUICK and the fifth-order WENO schemes for the spatial interpolation of the nonlinear fluxes. The fourth-order Runge-Kutta method advances the simulation in time.Findings: The simulations determine two parameters: the fractional growth rate of the linear instabilities; and the vorticity thickness of the first nonlinear peak. Grid refinement using 32, 64, 128, 256 and 512 nodes over one wave length determines the exact values by extrapolation and the computational error for the parameters. It also determines the overall order of convergence for each of the flux-limiting schemes used in the numerical simulations.Originality/value– The four-digit accuracy of the numerical simulations presented in this paper are comparable to analytical solutions. The development of this reliable numerical simulation method has paved the way for further study of the instabilities in shear flows that radiate waves
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