Wind generators are installed at sites with frequently continuous high wind speed, such as the interior United States and Atlantic coast of Northern Africa:
Portions of New Mexico are suitable for wind power, illustrated by purple areas on the preceding map. This section shows installation of a wind turbine in New Mexico in 2003. Newer wind turbines are even taller than this one.
To determine wind speed at heights above ground, a meteorological tower (met tower) may be installed at a wind farm.
Taller met towers are more expensive to build. To measure wind speed at greater heights, Sound Detection and Ranging (SODAR) may be used. SODAR is like the doppler sonar on ship hulls that measure water currents underneath, but pointing upward instead of downward.
The shapes of trees may be indicative of wind characteristics at a site:
Land topography affects wind flow. Higher wind speeds may be found above ridges (slightly after), and in gaps between ridges.
A wind vane on the wind turbine determines the wind direction and controls a motor that changes the direction of the turbine rotor to make sure it points into the wind.
The wind passing generally perpendicular through the rotor area forms a tube that widens after the rotor plane because the rotor has converted some of the wind speed to electricity, causing that tube of wind to slow down (bunch up) thus widening the stream tube downwind.
That widened air tube after the rotor is called the wake and eventually disperses into the atmosphere downstream. After the wake disperses, another turbine can be positioned to extract kinetic energy from the wind again. It must be far enough away to not be in the wake of the turbine in front of it.
The wake starts disappearing from the outer part of the air tube first. Thus, positioning a downstream turbine between upstream turbines (instead of directly behind another turbine) allows it to be less far downstream. This is possible if the wind direction is usually in only one direction.
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