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: https://doi.org/10.3402/tellusa.v22i1.10155 | Journal eISSN: 3035-9554
Language: English
Page range: 26 - 31
Submitted on: Aug 5, 1969
Published on: Jan 1, 1970
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1970 Hilding Sundqvist, George Veronis, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.