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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Main Authors: A. Sogachev, D. Cavar, M. Kelly, E. Dellwik, T. Klaas, P. Kühn
Format: Article
Language:English
Published: Copernicus Publications 2020-06-01
Series:Advances in Science and Research
Online Access:https://asr.copernicus.org/articles/17/53/2020/asr-17-53-2020.pdf
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spelling 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>&thinsp;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>&thinsp;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
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