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As a general rule, wind generators are practical where the average wind speed
is 10 mph (16 km/h or 4.5 m/s) or greater. Usually sites are pre-selected on
basis of a
wind atlas, and validated with wind measurements. Obviously,
meteorology plays an important part in determining possible locations for
wind parks, though it has great accuracy limitations. Meteorological wind data
is not usually sufficient for accurate siting of a large wind power project. An
'ideal' location would have a near constant flow of non-turbulent wind
throughout the year and would not suffer too many sudden powerful bursts of
wind. An important turbine siting factor is access to local demand or
transmission capacity.
Map of available wind power over the United States. Color codes indicate wind
power density class.
This map shows the wind resource in the United States. Land is categorized by
wind power class (left column of key), defined by a range of annual average wind
speeds measured at 10 meters (33 feet) and 50 meters (164 feet). The columns
called Wind Power estimate how much potential energy from the wind (in watts) is
available per square meter of land, assuming wind turbine hub height of 10 or 50
meters. (Of course, to calculate Wind Power, assumptions about turbine size and
performance were made.) Wind turbines are economical in wind power class 4–7.
The wind blows faster at higher altitudes because of the reduced influence of
drag of the surface (sea or land) and the reduced viscosity of the air. The
increase in velocity with altitude is most dramatic near the surface and is
affected by topography, surface roughness, and upwind obstacles such as trees or
buildings. Typically, the increase of wind speeds with increasing height follows
a logarithmic profile that can be reasonably approximated by the
wind profile power law, using an exponent of 1/7th, which predicts that wind
speed rises proportionally to the seventh root of altitude. Doubling the
altitude of a turbine, then, increases the expected wind speeds by 10% and the
expected power by 34% (calculation: increase in power = (2.0) ^(3/7) – 1 = 34%).
Wind farms or wind parks often have many turbines installed. Since each
turbine extracts some of the energy of the wind, it is important to provide
adequate spacing between turbines to avoid excess energy loss. Where land area
is sufficient, turbines are spaced three to five rotor diameters apart
perpendicular to the prevailing wind, and five to ten rotor diameters apart in
the direction of the prevailing wind, to minimize efficiency loss. The "wind
park effect" loss can be as low as 2% of the combined nameplate rating of
the turbines.
Utility-scale wind turbine generators have minimum temperature operating
limits which restrict the application in areas that routinely experience
temperatures less than −20°C. Wind turbines must be protected from ice
accumulation, which can make
anemometer readings inaccurate and which can cause high structure loads and
damage. Some turbine manufacturers offer low-temperature packages at a few
percent extra cost, which include internal heaters, different lubricants, and
different alloys for structural elements, to make it possible to operate the
turbines at lower temperatures. If the low-temperature interval is combined with
a low-wind condition, the wind turbine will require station service power,
equivalent to a few percent of its output rating, to maintain internal
temperatures during the cold snap. For example, the
St. Leon, Manitoba project has
a total rating of 99 MW and is estimated to need up to 3 MW (around 3% of
capacity) of station service power a few days a year for temperatures down to
−30°C. This factor affects the economics of wind turbine operation in cold
climates.
Onshore
Onshore turbine installations in hilly or mountainous regions tend to be on
ridgelines generally three kilometers or more inland from the nearest shoreline.
This is done to exploit the so-called topographic acceleration. The hill or
ridge causes the wind to accelerate as it is forced over it. The additional wind
speeds gained in this way make large differences to the amount of energy that is
produced. Great attention must be paid to the exact positions of the turbines (a
process known as micro-siting) because a difference of 30 m can sometimes mean a
doubling in output. Local winds are often monitored for a year or more with
anemometers and detailed wind maps constructed before wind generators are
installed.
For smaller installations where such data collection is too expensive or time
consuming, the normal way of
prospecting for wind-power sites is to directly look for trees or vegetation
that are permanently "cast" or deformed by the prevailing winds. Another way is
to use a wind-speed survey map, or historical data from a nearby meteorological
station, although these methods are less reliable.
Wind farm siting can sometimes be highly controversial, particularly as the
hilltop, often coastal sites preferred are often picturesque and environmentally
sensitive (for instance, having substantial bird life). Local residents in a
number of potential sites have strongly opposed the installation of wind farms,
and political support has resulted in the blocking of construction of some
installations.
Near-Shore
Near-Shore turbine installations are generally considered to be inside a zone
that is on land within three kilometers of a shoreline and on water within ten
kilometers of land. Wind speeds in these zones share wind speed characteristics
of both onshore wind and offshore wind depending on the prevailing wind
direction. Common issues that are shared within Near-shore wind development
zones are aviary (including bird migration and nesting), aquatic habitat,
transportation (including shipping and boating) and visual aesthetics amongst
several others.
Sea shores also tend to be windy areas and good sites for turbine
installation, because a primary source of wind is convection from the
differential heating and cooling of land and sea over the course of day and
night. Winds at sea level carry somewhat more energy than winds of the same
speed in mountainous areas because the air at sea level is more dense.
Near-shore wind farm siting can sometimes be highly controversial as coastal
sites are often picturesque and environmentally sensitive (for instance, having
substantial bird life). Local residents in a number of potential sites have
strongly opposed the installation of wind farms due to visual aesthetic
concerns.
Offshore
Offshore wind turbines near Copenhagen
Offshore wind development zones are generally considered to be ten kilometers
or more from land. Offshore wind turbines are less obtrusive than turbines on
land, as their apparent size and noise can be mitigated by distance. Because
water has less surface roughness than land (especially deeper water), the
average wind speed is usually considerably higher over open water. Capacity
factors (utilisation rates) are considerably higher than for onshore and
near-shore locations which allows offshore turbines to use shorter towers,
making them less visible.
In stormy areas with extended shallow continental shelves (such as Denmark),
turbines are practical to install — Denmark's wind generation provides about 18%
of total electricity demand in the country, with many offshore windfarms.
Denmark plans to increase wind energy's contribution to as much as half of its
electrical supply.
Locations have begun to be developed in the Great Lakes - with one project by
Trillium Power approximately 20 km from shore and over 700 MW in size. Ontario
is aggressively pursuing wind power development and has many onshore wind farms
and several proposed near-shore locations but presently only one offshore
development.
In most cases offshore environment is more expensive than onshore. Offshore
towers are generally taller than onshore towers once the submerged height is
included, and offshore foundations are more difficult to build and more
expensive. Power transmission from offshore turbines is generally through
undersea cable, which is more expensive to install than cables on land, and may
use high voltage direct current operation if significant distance is to be
covered — which then requires yet more equipment. Offshore saltwater
environments can also raise maintenance costs by corroding the towers, but
fresh-water locations such as the Great Lakes do not. Repairs and maintenance
are usually much more difficult, and generally more costly, than on onshore
turbines. Offshore saltwater wind turbines are outfitted with extensive
corrosion protection measures like coatings and cathodic protection, which may
not be required in fresh water locations.
While there is a significant market for small land-based windmills, offshore
wind turbines have recently been and will probably continue to be the largest
wind turbines in operation, because larger turbines allow for the spread of the
high fixed costs involved in offshore operation over a greater quantity of
generation, reducing the average cost. For similar reasons, offshore wind farms
tend to be quite large—often involving over 100 turbines—as opposed to onshore
wind farms which can operate competitively even with much smaller installations.