A multilevel method applied in the nonhomogeneous direction of the channel flow problem
β Scribed by F. Bouchon; F. Jauberteau
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 353 KB
- Volume
- 36
- Category
- Article
- ISSN
- 0168-9274
No coin nor oath required. For personal study only.
β¦ Synopsis
In this paper, we apply a spectral multilevel method in the nonhomogeneous direction of a channel. The spectral tau method being not well suited to separate the scales, we use a Galerkin basis in the wall normal direction. Then we can separate the scales, as in the periodic case, from the spectral decomposition of the velocity field. In this way, the quantities associated with the small and large scales verify the no slip boundary conditions. Then, we resolve the large and the small scale equations, simplifying the computation of the small scales. Indeed, we use a quasi-static approximation to compute the small scales. As for the interaction terms, we apply a quasi-static approximation to estimate the modulus, the phase being updated, at each time step, in function of the large scales. To validate the method proposed, we have done two simulations of the channel with the multilevel method. They correspond to two different choices of the total number of modes and of the coarse cut-off level for the multilevel method in the wall normal direction. The results obtained are compared with the results stemming from direct numerical simulations (DNS): one fine DNS (fine resolution) and one low DNS (coarse resolution).
π SIMILAR VOLUMES
In this article we introduce the separation of variables in the two-dimensional generalized Stokes problem, -Ξ½βu + Ξ±u + βp = f , for the flow in a channel. Also for the first time, we discuss the implementation of the Incremental Unknowns Method with a data structure of Compressed Column Storage. Tw
In the great hydraulic survey of the Mississippi river, conducted by Humphreys and Abbot, numerous velocity observations with double floats, were taken at different depths below the water surface. The combined results of all these observations are given on page 244 of the second edition of their \_R