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Journal of Wind Engineering
and Industrial Aerodynamics
journal homepage: www.elsevier.com/locate/jweia
Modeling of wind turbine wakes under thermally-stratified atmospheric
boundary layer
W.A. El-Askary
⁎
, I.M. Sakr, Ali M. AbdelSalam, M.R. Abuhegazy
Mechanical Power Engineering Department, Faculty of Engineering, Shebin El-Kom, Menoufia University, Egypt
ARTICLE INFO
Keywords:
Wind turbine wakes
Actuator disk
Atmospheric thermal stratification
Atmospheric boundary layer
RANS
k-ε model
Wind power
ABSTRACT
In the present work, the wake behavior of wind turbines, operating under thermally-stratified atmospheric
boundary layer (ABL), is numerically investigated. The steady state three dimensional Reynolds-Averaged
Navier–Stokes (RANS) equations, combined with the actuator disk approach, are used in the simulation. The
standard k-ε turbulence model as well as a modified one namely El Kasmi model are adopted. Two different
methods are used and compared, for representing the atmospheric stratification flow conditions: In the first one
(direct method), the energy equation is considered along with mass, momentum, and turbulence model
equations. In the second one (indirect method), stratification is modeled by means of additional buoyancy
production and dissipation terms. Such terms are added to the turbulent kinetic energy and dissipation rate
equations, instead of solving the energy equation. The results obtained from both methods show a reasonable
agreement with the experimental data available from the literature. Moreover, it is concluded that, there is no
significant difference between the predicted results from both methods. Further, the effect of the atmospheric
stability class on the wake deficit and the available wind power in the wake region has been also investigated
using the indirect method. It has been found that, there is a significant influence of the different atmospheric
conditions on the wake behavior. In particular, the wake region becomes smaller with the decreasing of
atmospheric stability, and hence a higher wind power in the wake region is observed for unstable conditions.
1. Introduction
Wind turbine wakes have attracted a lot of attention of the research
community in recent years because of their effect on power production
of wind farms. These wakes are characterized by a reduction of wind
speed which in turn reduces the available wind power, and an increase
of turbulence levels that generate fatigue loads on downstream wind
turbines. Therefore, the investigation of wind turbine wakes becomes
important to construct a suitable wind turbines farm.
Wind turbines operate in the lowest region of the atmospheric
boundary layer (ABL). Therefore, the evolution and recovery of wind
turbine wakes are strongly affected not only by the turbine character-
istics and complexity of terrain, but also, by the ambient wind speed
and turbulence levels related to the different thermal stratifications of
ABL. A proper modeling of all these factors becomes mandatory for
detailed understanding and accurate prediction of wind turbine wakes
and their effects on the performance of the whole wind farm. According
to the thermal conditions, the atmospheric boundary layer can be
classified into three types, which are neutral (NBL), stable (SBL), and
unstable or convective (CBL). In NBL, the mean potential temperature
is approximately constant with height, so that the generated turbulence
is mainly due to the ground surface. It is observed only during windy
weather with clouds. In SBL, the ground surface is colder than the
ambient air, therefore the generated turbulence by wind shear is
suppressed by negative buoyancy resulted from vertical downward
heat flux. This atmospheric condition usually occurs at night time. The
third type, CBL, occurs during day time when the ground surface is
warmer than ambient air. The vertical upward heat flux generates a
positive buoyancy, which in turn enhances the ambient turbulence. It is
observed that, the turbulence level varies in descending order of
magnitude in CBL, NBL and SBL, respectively.
Full-scale field measurements as well as wind tunnel experiments of
small-scaled models of wind turbines showed significant effects of
thermal stratification on wind power production and structure of wind-
turbine wakes, as reported in Van den Berg (2008), Wharton and
Lundquist (2010), Chamorro and Porté-Agel (2010), Zhang et al.
(2013), Hancock and Pascheke (2014). Baker and Walker (1984) used
a kite anemometer to measure wake deficits of two MOD-2, 2.5 MW,
91 m diameter wind turbines. The measurements were obtained at
different ambient turbulence levels under stable condition at Goodnoe
http://dx.doi.org/10.1016/j.jweia.2016.11.001
Received 29 April 2016; Received in revised form 31 October 2016; Accepted 5 November 2016
⁎
Corresponding author.
E-mail addresses: wageeh_elaskary@yahoo.com, Wageeh.Elaskary@sh-eng.menofia.edu.eg (W.A. El-Askary).
Journal of Wind Engineering & Industrial Aerodynamics 160 (2017) 1–15
Available online 16 November 2016
0167-6105/ © 2016 Elsevier Ltd. All rights reserved.
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