An Extension of Spectral Methods to Quasi-Periodic and Multiscale Problems
✍ Scribed by A. Wirth
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 385 KB
- Volume
- 132
- Category
- Article
- ISSN
- 0021-9991
No coin nor oath required. For personal study only.
✦ Synopsis
To give a first idea of our method consider a (quasiperiodic) function of one variable such that in its Fourier For efficiently treating quasi-periodic and multiscale problems numerically, it is here proposed to change the number of space representation the only wavenumbers present are of the dimensions which is then multiplied by the number of different form k ϭ n ϩ m, where n and m are signed integers and (incommensurable or widely separated) scales occurring in the is irrational (the decomposition of k is thus unique).
problem. Then, all calculations are performed in this higher-Such a function has the following (generalized) Fourier dimensional space. In the higher-dimensional space the problem and CPU resources, when using the ''higher dimension'' method, is typically proportional to the ratio of scales. ᮊ 1997 Academic Press such that f (x) is recovered by restriction to the line y ϭ x of slope .
📜 SIMILAR VOLUMES
## The operator A e = D 1 g 1 (x 1 / e,x 2 )D 1 +D 2 g 2 (x 1 / e,x 2 )D 2 is considered in L 2 (R 2 ), where g j (x 1 ,x 2 ), j = 1, 2, are periodic in x 1 with period 1, bounded and positive definite. Let function Q(x 1 ,x 2 ) be bounded, positive definite and periodic in x 1 with period 1. Let
Consider a triangular array \(X_{1}^{n}, \ldots, X_{n}^{n}, n \in \mathbb{N}\), of rowwise independent random clements with values in a measurable space. Suppose there exists \(\theta \in[0,1)\) such that \(X_{1}^{n}, \ldots, X_{\left.\left[n^{n}\right\}\right]}^{n}\) have distribution \(v_{1}\) and
## Abstract This paper studies the stability and numerical dispersion of an extension of the original finite‐difference time‐domain (FDTD) method to incorporate magnetized ferrites. This extension is based on discretizing the ferrite equations by means of central differences and averages. Both part