Interaction of Wind Turbine Wakes under Various Atmospheric Conditions

We present a numerical study of two utility-scale 5-MW turbines separated by seven rotor diameters. The effects of the atmospheric boundary layer flow on the turbine performance were assessed using large-eddy simulations. We found that the surface roughness and the atmospheric stability states had a...

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Main Authors: Sang Lee, Peter Vorobieff, Svetlana Poroseva
Format: Article
Language:English
Published: MDPI AG 2018-06-01
Series:Energies
Subjects:
Online Access:http://www.mdpi.com/1996-1073/11/6/1442
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spelling doaj-1ed2423f47c44ea98c7361e97ca056962020-11-25T01:48:28ZengMDPI AGEnergies1996-10732018-06-01116144210.3390/en11061442en11061442Interaction of Wind Turbine Wakes under Various Atmospheric ConditionsSang Lee0Peter Vorobieff1Svetlana Poroseva2Department of Mechanical Engineering, University of New Mexico, Albuquerque, NM 87131, USADepartment of Mechanical Engineering, University of New Mexico, Albuquerque, NM 87131, USADepartment of Mechanical Engineering, University of New Mexico, Albuquerque, NM 87131, USAWe present a numerical study of two utility-scale 5-MW turbines separated by seven rotor diameters. The effects of the atmospheric boundary layer flow on the turbine performance were assessed using large-eddy simulations. We found that the surface roughness and the atmospheric stability states had a profound effect on the wake diffusion and the Reynolds stresses. In the upstream turbine case, high surface roughness increased the wind shear, accelerating the decay of the wake deficit and increasing the Reynolds stresses. Similarly, atmospheric instabilities significantly expedited the wake decay and the Reynolds stress increase due to updrafts of the thermal plumes. The turbulence from the upstream boundary layer flow combined with the turbine wake yielded higher Reynolds stresses for the downwind turbine, especially in the streamwise component. For the downstream turbine, diffusion of the wake deficits and the sharp peaks in the Reynolds stresses showed faster decay than the upwind case due to higher levels of turbulence. This provides a physical explanation for how turbine arrays or wind farms can operate more efficiently under unstable atmospheric conditions, as it is based on measurements collected in the field.http://www.mdpi.com/1996-1073/11/6/1442atmospheric boundary layerwind turbinesenergy capture
collection DOAJ
language English
format Article
sources DOAJ
author Sang Lee
Peter Vorobieff
Svetlana Poroseva
spellingShingle Sang Lee
Peter Vorobieff
Svetlana Poroseva
Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
Energies
atmospheric boundary layer
wind turbines
energy capture
author_facet Sang Lee
Peter Vorobieff
Svetlana Poroseva
author_sort Sang Lee
title Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
title_short Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
title_full Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
title_fullStr Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
title_full_unstemmed Interaction of Wind Turbine Wakes under Various Atmospheric Conditions
title_sort interaction of wind turbine wakes under various atmospheric conditions
publisher MDPI AG
series Energies
issn 1996-1073
publishDate 2018-06-01
description We present a numerical study of two utility-scale 5-MW turbines separated by seven rotor diameters. The effects of the atmospheric boundary layer flow on the turbine performance were assessed using large-eddy simulations. We found that the surface roughness and the atmospheric stability states had a profound effect on the wake diffusion and the Reynolds stresses. In the upstream turbine case, high surface roughness increased the wind shear, accelerating the decay of the wake deficit and increasing the Reynolds stresses. Similarly, atmospheric instabilities significantly expedited the wake decay and the Reynolds stress increase due to updrafts of the thermal plumes. The turbulence from the upstream boundary layer flow combined with the turbine wake yielded higher Reynolds stresses for the downwind turbine, especially in the streamwise component. For the downstream turbine, diffusion of the wake deficits and the sharp peaks in the Reynolds stresses showed faster decay than the upwind case due to higher levels of turbulence. This provides a physical explanation for how turbine arrays or wind farms can operate more efficiently under unstable atmospheric conditions, as it is based on measurements collected in the field.
topic atmospheric boundary layer
wind turbines
energy capture
url http://www.mdpi.com/1996-1073/11/6/1442
work_keys_str_mv AT sanglee interactionofwindturbinewakesundervariousatmosphericconditions
AT petervorobieff interactionofwindturbinewakesundervariousatmosphericconditions
AT svetlanaporoseva interactionofwindturbinewakesundervariousatmosphericconditions
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