A simple finite-difference grid with non-constant intervals
Open Access
- 1 February 1970
- journal article
- Published by Stockholm University Press in Tellus
- Vol. 22 (1), 26-31
- https://doi.org/10.1111/j.2153-3490.1970.tb01933.x
Abstract
A finite difference network with non-uniform grid intervals, hi, such that hi = hi-1 + O(h2i-1) is presented. The use of the grid network for two specific choices of hi - hi-1 for a linear boundary layer problem shows that it has distinct advantages in computational efficiency and in accuracy of representation of the analytical solution. DOI: 10.1111/j.2153-3490.1970.tb01933.xKeywords
This publication has 1 reference indexed in Scilit:
- The westward intensification of wind‐driven ocean currentsEOS, Transactions American Geophysical Union, 1948