In a wind farm or wind power plant,
individual turbines are interconnected with a medium voltage (often 34.5 kV),
power collection system and communications network. At a substation, this
medium-voltage electrical current is increased in voltage with a transformer
for connection to the high voltage electric power transmission system.
The surplus power produced by domestic microgenerators can,
in some jurisdictions, be fed into the network and sold to the utility company,
producing a retail credit for the microgenerators' owners to offset their
energy costs.
Induction generators, often used for wind power plant,
require reactive power for excitation so substations used in wind-power
collection systems include substantial capacitor banks for power factor
correction. Different types of wind turbine generators behave differently
during transmission grid disturbances, so extensive modelling of the dynamic
electromechanical characteristics of a new wind farm is required by
transmission system operators to ensure predictable stable behaviour during
system faults. In particular, induction generators cannot support the system
voltage during faults, unlike steam or hydro turbine-driven synchronous
generators. Doubly-fed machines—wind turbines with solid-state converters
between the turbine generator and the collector system—generally have more
desirable properties for grid interconnection. Transmission systems operators
will supply a wind farm developer with a grid code to specify
the requirements for interconnection to the transmission grid. This will
include power factor, constancy of frequency and dynamic behavior of the wind
farm turbines during a system fault.
Since wind speed is not constant, a wind farm's annual energy
production is never as much as the sum of the generator nameplate ratings
multiplied by the total hours in a year. The ratio of actual productivity in a
year to this theoretical maximum is called the capacity factor. Typical
capacity factors are 20–40%, with values at the upper end of the range in
particularly favorable sites. For example, a 1 MW turbine with a capacity
factor of 35% will not produce 8,760 MW·h in a year (1 × 24 × 365), but only 1
× 0.35 × 24 × 365 = 3,066 MW·h, averaging to 0.35 MW. Online data is available
for some locations and the capacity factor can be calculated from the yearly
output.
Unlike fueled generating plants, the capacity factor is
limited by the inherent properties of wind. Capacity factors of other types ofwind
power plant are based mostly on fuel cost, with a small amount of
downtime for maintenance. Nuclear plants have low incremental fuel cost, and so
are run at full output and achieve a 90% capacity factor. Plants with higher
fuel cost are throttled back to follow load. Gas turbine plants using natural
gas as fuel may be very expensive to operate and may be run only to meet peak
power demand. A gas turbine plant may have an annual capacity factor of 5–25%
due to relatively high energy production cost.
According to a 2007 Stanford University study published in
the Journal of Applied Meteorology and Climatology, interconnecting ten or more
wind farms can allow an average of 33% of the total energy produced to be used
as reliable, baseload electric power, as long as minimum criteria are met for
wind speed and turbine height.
In a 2008 study released by the U.S. Department of Energy's
Office of Energy Efficiency and Renewable Energy, the capacity factor achieved
by the wind turbine fleet is shown to be increasing as the technology improves.
The capacity factor achieved by new wind turbines in 2004 and 2005 reached 36%.
Wind energy "penetration" refers to the fraction of energy produced
by wind compared with the total available generation capacity. There is no
generally accepted "maximum" level of wind penetration. The limit for
a particular grid will depend on the existing generating plants, pricing
mechanisms, capacity for storage or demand management, and other factors. An
interconnected electricity grid will already include reserve generating and
transmission capacity to allow for equipment failures; this reserve capacity
can also serve to regulate for the varying power generation by wind
power plants. Studies have indicated that 20% of the total electrical
energy consumption may be incorporated with minimal difficulty. These studies
have been for locations with geographically dispersed wind farms, some degree
of dispatchable energy, or hydropower with storage capacity, demand management,
and interconnection to a large grid area export of electricity when needed.
Beyond this level, there are few technical limits, but the economic
implications become more significant. Electrical utilities continue to study
the effects of large (20% or more) scale penetration of wind generation on
system stability and economics.
At present, a few grid systems have penetration of wind
energy above 5%: Denmark (values over 19%), Spain and Portugal (values over
11%), Germany and the Republic of Ireland (values over 6%). For instance, in
the morning hours of 8 November 2009, wind energy produced covered more than
half the electricity demand in Spain, setting a new record, and without
problems for the network.
The Danish grid is heavily interconnected to the European
electrical grid, and it has solved grid management problems by exporting almost
half of its wind power to Norway. The correlation between electricity export
and wind power production is very strong.
Electricity generated
from wind power plant can be highly variable at several
different timescales: from hour to hour, daily, and seasonally. Annual
variation also exists, but is not as significant. Related to variability is the
short-term (hourly or daily) predictability of wind plant output. Like other
electricity sources, wind energy must be "scheduled". Wind power
forecasting methods are used, but predictability of wind plant output remains
low for short-term operation.
Because instantaneous electrical generation and consumption
must remain in balance to maintain grid stability, this variability can present
substantial challenges to incorporating large amounts of wind power into a grid
system. Intermittency and the non-dispatchable nature of wind energy production
can raise costs for regulation, incremental operating reserve, and (at high
penetration levels) could require an increase in the already existing energy
demand management, load shedding, or storage solutions or system
interconnection with HVDC cables. At low levels of wind penetration, fluctuations
in load and allowance for failure of large generating units requires reserve
capacity that can also regulate for variability of wind generation. Wind power
can be replaced by other power stations during low wind periods. Transmission
networks must already cope with outages of generation plant and daily changes
in electrical demand. Systems with large wind capacity components may need more
spinning reserve (plants operating at less than full load).
Pumped-storage hydroelectricity or other forms of grid energy
storage can store energy developed by high-wind periods and release it when
needed. Stored energy increases the economic value of wind energy since
it can be shifted to displace higher cost generation during peak demand
periods. The potential revenue from this arbitrage can offset the cost and
losses of storage; the cost of storage may add 25% to the cost of any wind
energy stored, but it is not envisaged that this would apply to a large
proportion of wind energy generated. The 2 GW Dinorwig pumped storage plant in
Wales evens out electrical demand peaks, and allows base-load suppliers to run
their plant more efficiently. Although pumped storage power systems are only
about 75% efficient, and have high installation costs, their low running costs
and ability to reduce the required electrical base-load can save both fuel and
total electrical generation costs.
In particular geographic regions, peak wind speeds may not
coincide with peak demand for electrical power. In the US states of California
and Texas, for example, hot days in summer may have low wind speed and high
electrical demand due to air conditioning. Some utilities subsidize the
purchase of geothermal heat pumps by their customers, to reduce electricity
demand during the summer months by making air conditioning up to 70% more
efficient; widespread adoption of this technology would better match
electricity demand to wind availability in areas with hot summers and low
summer winds. Another option is to interconnect widely dispersed geographic areas
with an HVDC "Super grid". In the USA it is estimated that to upgrade
the transmission system to take in planned or potential renewables would cost
at least $60 billion. Total annual US power consumption in 2006 was 4 thousand
billion kW·h. Over an asset life of 40 years and low cost utility investment
grade funding, the cost of $60 billion investment would be about 5% p.a. (i.e.
$3 billion p.a.) Dividing by total power used gives an increased unit cost of
around $3,000,000,000 × 100 / 4,000 × 1 exp9 = 0.075 cent/kW·h.
In the UK, demand for electricity is higher in winter than in
summer, and so are wind speeds. Solar power tends to be complementary to wind.
On daily to weekly timescales, high pressure areas tend to bring clear skies
and low surface winds, whereas low pressure areas tend to be windier and
cloudier. On seasonal timescales, solar energy typically peaks in summer,
whereas in many areas wind energy is lower in summer and higher in winter. Thus
the intermittencies of wind and solar power tend to cancel each other somewhat.
A demonstration project at the Massachusetts Maritime Academy shows the effect.
The Institute for Solar Energy Supply Technology of the University of Kassel
pilot-tested a combined power plant linking solar, wind, biogas and
hydrostorage to provide load-following power around the clock, entirely from
renewable sources.
A report from Denmark noted that their wind power network was
without power for 54 days during 2002. Wind power advocates argue that these
periods of low wind can be dealt with by simply restarting existing power
stations that have been held in readiness or interlinking with HVDC. Electrical
grids with slow-responding thermal power plants and without ties to networks
with hydroelectric generation may have to limit the use of wind power.
Three reports on the wind variability in the UK issued in
2009, generally agree that variability of wind needs to be taken into account,
but it does not make the grid unmanageable; and the additional costs, which are
modest, can be quantified.
A 2006 International Energy Agency forum presented costs for
managing intermittency as a function of wind-energy's share of total capacity
for several countries, as shown:
Increase in system
operation costs, Euros per MW·h, for 10% and 20% wind share
|
10% |
20% |
Germany |
2.5 |
3.2 |
Denmark |
0.4 |
0.8 |
Finland |
0.3 |
1.5 |
Norway |
0.1 |
0.3 |
Sweden |
0.3 |
0.7 |
Many commentators concentrate on whether or not wind has any
"capacity credit" without defining what they mean by this and its
relevance. Wind does have a capacity credit, using a widely accepted and
meaningful definition, equal to about 20% of its rated output (but this figure
varies depending on actual circumstances). This means that reserve capacity on
a system equal in MW to 20% of added wind could be retired when such wind is
added without affecting system security or robustness. But the precise value is
irrelevant since the main value of wind (in the UK, worth 5 times the capacity
credit value) is its fuel and CO2 savings.