Flow Adjustment Inside and Around Large Finite-Size Wind Farms

Energies 2017, 10(12), 2164; doi:10.3390/en10122164

Article: Flow Adjustment Inside and Around Large Finite-Size Wind Farms

In this study, large-eddy simulations are performed to investigate the flow inside and around large finite-size wind farms in conventionally-neutral atmospheric boundary layers. Special emphasis is placed on characterizing the different farm-induced flow regions, including the induction, entrance and development, fully-developed, exit and farm wake regions. The wind farms extend 20 km in the streamwise direction and comprise 36 wind turbine rows arranged in aligned and staggered configurations. Results show that, under weak free-atmosphere stratification (Γ=1 K/km), the flow inside and above both wind farms, and thus the turbine power, do not reach the fully-developed regime even though the farm length is two orders of magnitude larger than the boundary layer height. In that case, the wind farm induction region, affected by flow blockage, extends upwind about 0.8 km and leads to a power reduction of 1.3% and 3% at the first row of turbines for the aligned and staggered layouts, respectively. The wind farm wake leads to velocity deficits at hub height of around 3.5% at a downwind distance of 10 km for both farm layouts. Under stronger stratification (Γ=5 K/km), the vertical deflection of the subcritical flow induced by the wind farm at its entrance and exit regions triggers standing gravity waves whose effects propagate upwind. They, in turn, induce a large decelerating induction region upwind of the farm leading edge, and an accelerating exit region upwind of the trailing edge, both extending about 7 km. As a result, the turbine power output in the entrance region decreases more than 35% with respect to the weakly stratified case. It increases downwind as the flow adjusts, reaching the fully-developed regime only for the staggered layout at a distance of about 8.5 km from the farm edge. The flow acceleration in the exit region leads to an increase of the turbine power with downwind distance in that region, and a relatively fast (compared with the weakly stratified case) recovery of the farm wake, which attains its inflow hub height speed at a downwind distance of 5 km.

Keywords: atmospheric boundary layer (ABL); boundary-layer depth; exit region; farm wake; induction region; large-eddy simulation (LES); large finite-size wind farm; turbulence

Flow adjustment regions in large finite-size wind farms in CNBLs with (a) weak and (b) strong free-atmosphere stratification.
Screen Shot 2018-02-09 at 12.16.20
Contours of time-averaged horizontal velocity magnitude M on the xz plane through the center of a wind turbine column for the case (a) FS−aΓ1; (b) FS−sΓ1; (c) FS−aΓ5; (d) FS−sΓ5.

Authors: Ka Ling Wu [EPFL], Fernando Porté-Agel [EPFL]


Leave a Reply

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out /  Change )

Facebook photo

You are commenting using your Facebook account. Log Out /  Change )

Connecting to %s

Blog at WordPress.com.

%d bloggers like this: