## Abstract A numerical model of the local flow above an infinite series of two dimensional ridges is used to investigate the extent to which form drag on the ridges is balanced by reductions in surface shear stress compared to that for a plane surface. With a constant eddy viscosity Mason and Syke
A simple model of neutrally stratified boundary-layer flow over real terrain incorporating wavenumber-dependent scaling
โ Scribed by P. A. Taylor; J. L. Walmsley; J. R. Salmon
- Publisher
- Springer
- Year
- 1983
- Tongue
- English
- Weight
- 1008 KB
- Volume
- 26
- Category
- Article
- ISSN
- 0006-8314
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โฆ Synopsis
Our experience in applying earlier versions of a model of boundary-layer flow over low hills to real terrain (see Walmsley et al., 1982) has led to the development of a new version which we designate MS3DJH/3. The main improvements are the use of terrain-dependent length and velocity scales and the blending of inner and outer layer results into a single 'universally valid' solution for the velocity perturbation field. MS3DJH/3 was carefully calibrated against alternative computations of Row over idealized twodimensional terrain features using more detailed models prior to its application to real, three-dimensional terrain. It still provides high spatial resolution with low computing cost and is applicable to flow over terrain features with horizontal scales from 10 m to 10 km.
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