Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements

Vertical profiles of the horizontal wind speed and of the standard deviation of vertical wind speed from Large Eddy Simulations of a convective atmospheric boundary layer are compared to wind LIDAR measurements up to 1400 m. Fair agreement regarding both types of profiles is observed only when the s...

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Main Authors: J. G. Pedersen, M. Kelly, S.-E. Gryning, R. Floors, E. Batchvarova, A. Peña
Format: Article
Language:English
Published: Copernicus Publications 2012-04-01
Series:Advances in Science and Research
Online Access:http://www.adv-sci-res.net/8/83/2012/asr-8-83-2012.pdf
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spelling doaj-f2f5b097c3d54adfb542082b8e23ffa12020-11-24T21:23:09ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362012-04-018838610.5194/asr-8-83-2012Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurementsJ. G. Pedersen0M. Kelly1S.-E. Gryning2R. Floors3E. Batchvarova4A. Peña5Department of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkDepartment of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkDepartment of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkDepartment of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkDepartment of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkDepartment of Wind Energy, Risø Campus, Technical University of Denmark, Roskilde, DenmarkVertical profiles of the horizontal wind speed and of the standard deviation of vertical wind speed from Large Eddy Simulations of a convective atmospheric boundary layer are compared to wind LIDAR measurements up to 1400 m. Fair agreement regarding both types of profiles is observed only when the simulated flow is driven by a both time- and height-dependent geostrophic wind and a time-dependent surface heat flux. This underlines the importance of mesoscale effects when the flow above the atmospheric surface layer is simulated with a computational fluid dynamics model.http://www.adv-sci-res.net/8/83/2012/asr-8-83-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. G. Pedersen
M. Kelly
S.-E. Gryning
R. Floors
E. Batchvarova
A. Peña
spellingShingle J. G. Pedersen
M. Kelly
S.-E. Gryning
R. Floors
E. Batchvarova
A. Peña
Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
Advances in Science and Research
author_facet J. G. Pedersen
M. Kelly
S.-E. Gryning
R. Floors
E. Batchvarova
A. Peña
author_sort J. G. Pedersen
title Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
title_short Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
title_full Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
title_fullStr Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
title_full_unstemmed Comparison of Large Eddy Simulations of a convective boundary layer with wind LIDAR measurements
title_sort comparison of large eddy simulations of a convective boundary layer with wind lidar measurements
publisher Copernicus Publications
series Advances in Science and Research
issn 1992-0628
1992-0636
publishDate 2012-04-01
description Vertical profiles of the horizontal wind speed and of the standard deviation of vertical wind speed from Large Eddy Simulations of a convective atmospheric boundary layer are compared to wind LIDAR measurements up to 1400 m. Fair agreement regarding both types of profiles is observed only when the simulated flow is driven by a both time- and height-dependent geostrophic wind and a time-dependent surface heat flux. This underlines the importance of mesoscale effects when the flow above the atmospheric surface layer is simulated with a computational fluid dynamics model.
url http://www.adv-sci-res.net/8/83/2012/asr-8-83-2012.pdf
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