Abstract
A simplified model for a weakly unstable atmospheric boundary layer capped by a stable inversion layer at the top is presented. This type of boundary layer flow might occur frequently over high-latitude ice fields for sufficiently strong winds. The shear stress is modelled by using a linear eddy viscosity representation. The vertical boundary layer structure, the associated surface shear stress and surface shear stress direction are presented together with comparison with a data set from field observations.
Original language | English (US) |
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Pages (from-to) | 123-139 |
Number of pages | 17 |
Journal | Journal of Wind Engineering and Industrial Aerodynamics |
Volume | 37 |
Issue number | 2 |
DOIs | |
State | Published - Mar 1991 |
Externally published | Yes |
ASJC Scopus subject areas
- Civil and Structural Engineering
- Renewable Energy, Sustainability and the Environment
- Mechanical Engineering