A finite element model for the study of heated island effects
DOI:
https://doi.org/10.54302/mausam.v33i3.2818Abstract
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.
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