Year: 1982
Type: article
Abstract: Steady state solutions for the nonlinear equations which govern planetary boundary layer flow is obtained through finite element method as well as by the usual finite difference technique. The physical phenomenon corresponds to that of a flowover a surface varying in surface roughness and temperature along one direction. Comparison of the results show a good agreement between the two techniques employed.
Source: MAUSAM
Authors: N. RAMANATHAN, R. NATARAJAN
Institution: Indian Institute of Technology Delhi
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: diamond
OpenAlex ID: W3204432604