Abstract
A three-dimensional mesoscale meteorological model was developed based on second-moment closure equations that were solved by the finite-element method. This paper aims to evaluate the performance of the model under flat terrain and horizontally homogeneous atmospheric boundary layer conditions. The one-dimensional version of this model was tested against field measurements, a water tank experiment, and another numerical model. It showed several interesting behaviors of the atmospheric boundary layer under stable and unstable flows that are of primary interest for environmental studies.
Corresponding author address: Dr. D. Y. C. Leung, Department of Mechanical Engineering, 7/F, Haking Wong Building, University of Hong Kong, Pokfulam Road, Hong Kong, China.