Numerical modelling of the wind over forests: roughness versus canopy drag
<p>Parameterizing the effect of vertically-distributed vegetation through an effective roughness (<span class="inline-formula"><i>z</i><sub>0,eff</sub></span>) – whereby momentum loss through a three-dimensional foliage volume is represented as mom...
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doaj-4087f4a124a54b9d925a880aaad94b052020-11-25T02:39:55ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362020-06-0117536110.5194/asr-17-53-2020Numerical modelling of the wind over forests: roughness versus canopy dragA. Sogachev0D. Cavar1M. Kelly2E. Dellwik3T. Klaas4P. Kühn5Wind Energy Department, Technical University of Denmark, Roskilde, DenmarkWind Energy Department, Technical University of Denmark, Roskilde, DenmarkWind Energy Department, Technical University of Denmark, Roskilde, DenmarkWind Energy Department, Technical University of Denmark, Roskilde, DenmarkFraunhofer IEE, Königstor 59, 34119 Kassel, GermanyFraunhofer IEE, Königstor 59, 34119 Kassel, Germany<p>Parameterizing the effect of vertically-distributed vegetation through an effective roughness (<span class="inline-formula"><i>z</i><sub>0,eff</sub></span>) – whereby momentum loss through a three-dimensional foliage volume is represented as momentum loss over an area at one vertical level – can facilitate the use of forest data in flow models, to any level of detail, and simultaneously reduce computational cost. Results of numerical experiments and comparison with observations show that a modelling approach based on <span class="inline-formula"><i>z</i><sub>0,eff</sub></span> can estimate wind speed and turbulence levels over forested areas, at heights of interest for wind energy applications (<span class="inline-formula">∼60</span> m and higher), but only above flat terrain. Caution must be exercised in the application of such a model to zones of forest edges. Advanced flow models capable of incorporating local (distributed) drag forces are recommended for complex terrain covered by forest.</p>https://asr.copernicus.org/articles/17/53/2020/asr-17-53-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. Sogachev D. Cavar M. Kelly E. Dellwik T. Klaas P. Kühn |
spellingShingle |
A. Sogachev D. Cavar M. Kelly E. Dellwik T. Klaas P. Kühn Numerical modelling of the wind over forests: roughness versus canopy drag Advances in Science and Research |
author_facet |
A. Sogachev D. Cavar M. Kelly E. Dellwik T. Klaas P. Kühn |
author_sort |
A. Sogachev |
title |
Numerical modelling of the wind over forests: roughness versus canopy drag |
title_short |
Numerical modelling of the wind over forests: roughness versus canopy drag |
title_full |
Numerical modelling of the wind over forests: roughness versus canopy drag |
title_fullStr |
Numerical modelling of the wind over forests: roughness versus canopy drag |
title_full_unstemmed |
Numerical modelling of the wind over forests: roughness versus canopy drag |
title_sort |
numerical modelling of the wind over forests: roughness versus canopy drag |
publisher |
Copernicus Publications |
series |
Advances in Science and Research |
issn |
1992-0628 1992-0636 |
publishDate |
2020-06-01 |
description |
<p>Parameterizing the effect of vertically-distributed vegetation
through an effective roughness (<span class="inline-formula"><i>z</i><sub>0,eff</sub></span>) – whereby momentum
loss through a three-dimensional foliage volume is represented as momentum
loss over an area at one vertical level – can facilitate the use of forest
data in flow models, to any level of detail, and simultaneously reduce
computational cost. Results of numerical experiments and comparison with
observations show that a modelling approach based on <span class="inline-formula"><i>z</i><sub>0,eff</sub></span> can estimate wind speed and turbulence levels over
forested areas, at heights of interest for wind energy applications
(<span class="inline-formula">∼60</span> m and higher), but only above flat terrain. Caution must
be exercised in the application of such a model to zones of forest edges.
Advanced flow models capable of incorporating local (distributed) drag
forces are recommended for complex terrain covered by forest.</p> |
url |
https://asr.copernicus.org/articles/17/53/2020/asr-17-53-2020.pdf |
work_keys_str_mv |
AT asogachev numericalmodellingofthewindoverforestsroughnessversuscanopydrag AT dcavar numericalmodellingofthewindoverforestsroughnessversuscanopydrag AT mkelly numericalmodellingofthewindoverforestsroughnessversuscanopydrag AT edellwik numericalmodellingofthewindoverforestsroughnessversuscanopydrag AT tklaas numericalmodellingofthewindoverforestsroughnessversuscanopydrag AT pkuhn numericalmodellingofthewindoverforestsroughnessversuscanopydrag |
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