New insights on wind turbine wakes from large‐eddy simulation: Wake contraction, dual nature, and temperature effects

• Published in: Wind energy (Chichester, England) Vol. 27; no. 11; pp. 1130 - 1151
• Main Authors: Wu, Sicheng, Archer, Cristina L., Mirocha, Jeffrey D.
• Format: Journal Article
• Language: English
• Published: Bognor Regis John Wiley & Sons, Inc 01-11-2024; Wiley Blackwell (John Wiley & Sons); Wiley
• Subjects: Actuators; Aerodynamics; ENVIRONMENTAL SCIENCES; Heat flux; Kinetic energy; Large eddy simulation; Rotors; Similarity theory; Stability; temperature; Temperature effects; Turbines; turbulence kinetic energy; Turbulent wind; Vortices; wake expansion; Wakes; Weather forecasting; Wind effects; WIND ENERGY; Wind measurement; Wind power; Wind speed; wind speed deficit; wind turbine wake; Wind turbines
• ISSN: 1095-4244; 1099-1824
• DOI: 10.1002/we.2827

Large‐eddy simulation (LES) has been adopted to study wind turbine wakes because it can capture fine‐scale details of turbulent wind flows and interactions with wind turbines. Here, we use the LES version of the Weather Research and Forecasting (WRF) model with an actuator disk model to gain insights on several wake effects that have been traditionally difficult to measure. The first finding is that the wake has a “dual nature,” meaning that the wind speed deficit behaves differently from the added turbulent kinetic energy (TKE) and the two are not co‐located in space. For example, the wind speed deficit peaks at hub height and reaches the ground within 8D (D is the rotor diameter), but added TKE peaks near the rotor tip and generally remains aloft. Second, temperature changes near the ground are driven by the added TKE in the rotor area and by atmospheric stability. The combination of these two factors determines the sign and intensity of the vertical heat flux divergence below the rotor, with convergence and warming associated with stable conditions and weak divergence and modest cooling with unstable conditions. Third, wakes do not expand indefinitely, as suggested by similarity theory applied to the wind speed deficit, but eventually stop expanding and actually contract, at different rates depending on atmospheric stability. The implication of these findings is that, in order to study wakes, it is not sufficient to focus on wind speed deficit alone, because TKE is also important and yet behaves differently from the wind speed deficit.