An Analytical Model for the Regeneration of Wind after Exiting a Wind Farm
The simplest model for an atmospheric boundary layer assumes a uniform steady wind over a certain depth, of order 1 km, with the forces of friction, pressure gradient and Coriolis in balance. A linear model is here employed for the adjustment of wind to this equilibrium, as the wake of a very wide w...
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
MDPI AG
2018-08-01
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| Col·lecció: | Energies |
| Matèries: | |
| Accés en línia: | http://www.mdpi.com/1996-1073/11/8/2071 |
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