Parameterization of convective and stable internal boundary layers into mass consistent models
Identifieur interne : 000260 ( Main/Exploration ); précédent : 000259; suivant : 000261Parameterization of convective and stable internal boundary layers into mass consistent models
Auteurs : F. Castino [Grèce] ; M. Tombrou [Grèce]Source :
- Journal of Wind Engineering & Industrial Aerodynamics [ 0167-6105 ] ; 1998.
English descriptors
- KwdEn :
- Aerodyn, Boundary layer, Boundary layer meteorol, Castino, Coastal regions, Complex topography, Elsevier science, Initial wind, Internal boundary layer, Nisyros island, Obukhov length, Planetary boundary layer, Roughness, Roughness change, Roughness length, Stability conditions, Surface elevation, Surface roughness, Surface roughness change, Surface temperature, Typical values, Unstable case, Unstable conditions, Upwind conditions, Velocity modulus, Wind direction, Wind speed.
- Teeft :
- Aerodyn, Boundary layer, Boundary layer meteorol, Castino, Coastal regions, Complex topography, Elsevier science, Initial wind, Internal boundary layer, Nisyros island, Obukhov length, Planetary boundary layer, Roughness, Roughness change, Roughness length, Stability conditions, Surface elevation, Surface roughness, Surface roughness change, Surface temperature, Typical values, Unstable case, Unstable conditions, Upwind conditions, Velocity modulus, Wind direction, Wind speed.
Abstract
Abstract: Feasibility studies for the deployment of wind turbines and for air quality analysis in coastal regions require detailed knowledge of wind climatology in this area. In practice, however, the information available is very limited. Thus, the improvement of the physical modelling in the existing relatively simple micrositing models seems to be a good compromise between desired accuracy (and reliability) and required computer resources and expertise. In this work, simple parameterizations of the IBL concept, in a first step due to the effect of a change in surface roughness and in a second step taking into account a change in surface temperature, have been introduced in a mass consistent model. For the validation of the model, data of wind speed at 10m height at three locations, from a wind field experiment over a complex topography, were used, showing a satisfactory model improvement.
Url:
DOI: 10.1016/S0167-6105(98)00021-X
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000049
- to stream Istex, to step Curation: 000049
- to stream Istex, to step Checkpoint: 000197
- to stream Main, to step Merge: 000266
- to stream Main, to step Curation: 000260
Le document en format XML
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<term>Roughness change</term>
<term>Roughness length</term>
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<term>Surface roughness</term>
<term>Surface roughness change</term>
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<term>Typical values</term>
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<front><div type="abstract" xml:lang="en">Abstract: Feasibility studies for the deployment of wind turbines and for air quality analysis in coastal regions require detailed knowledge of wind climatology in this area. In practice, however, the information available is very limited. Thus, the improvement of the physical modelling in the existing relatively simple micrositing models seems to be a good compromise between desired accuracy (and reliability) and required computer resources and expertise. In this work, simple parameterizations of the IBL concept, in a first step due to the effect of a change in surface roughness and in a second step taking into account a change in surface temperature, have been introduced in a mass consistent model. For the validation of the model, data of wind speed at 10m height at three locations, from a wind field experiment over a complex topography, were used, showing a satisfactory model improvement.</div>
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