Comments and further analysis on effective roughness lengths for use in numerical three-dimensional models

Details Comments and further analysis on effective roughness lengths for use in numerical three-dimensional models Comments and further analysis on effective roughness lengths for use in numerical three-dimensional models

Jun 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987bolme..39..403t&link_type=abstract

Boundary-Layer Meteorology (ISSN 0006-8314), vol. 39, no. 4, June 1987, p. 403-418; Reply, p. 419.

Physics

35

Atmospheric Models, Boundary Layer Flow, Micrometeorology, Planetary Boundary Layer, Surface Roughness Effects, Terrain, Three Dimensional Models, Atmospheric Stratification, Flow Distribution, Perturbation Theory, Scale Models

Scientific paper

Simple calculations of the apparent roughness length for the areally
averaged flow over flat but heterogeneous terrain are presented. These
results could be used to specify effective roughness lengths for use in
large-scale models. Some of our conclusions differ significantly from
those reached recently by Andre and Blondin (1986).

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