Wind gradient
In common usage, wind gradient, more specifically wind speed gradient[1] or wind velocity gradient,[2] or alternatively shear wind,[3] is the vertical component of the
Simple explanation
Characterization
Typically, due to
The reduction in velocity near the surface is a function of surface roughness. Wind velocity profiles are quite different for different terrain types.[8] Rough, irregular ground, and man-made obstructions on the ground, retard movement of the air near the surface, reducing wind velocity.[4][11] Because of the relatively smooth water surface, wind speeds do not decrease as much close to the sea as they do on land.[12] Over a city or rough terrain, the wind gradient effect could cause a reduction of 40% to 50% of the geostrophic wind speed aloft; while over open water or ice, the reduction may be only 20% to 30%.[13][14]
For
Although the power law exponent approximation is convenient, it has no theoretical basis.
The shearing of the wind is usually three-dimensional,[21] that is, there is also a change in direction between the 'free' pressure-driven geostrophic wind and the wind close to the ground.[22] This is related to the Ekman spiral effect. The cross-isobar angle of the diverted ageostrophic flow near the surface ranges from 10° over open water, to 30° over rough hilly terrain, and can increase to 40°-50° over land at night when the wind speed is very low.[14]
After sundown the wind gradient near the surface increases, with the increasing stability.[23] Atmospheric stability occurring at night with radiative cooling tends to contain turbulent eddies vertically, increasing the wind gradient.[10] The magnitude of the wind gradient is largely influenced by the height of the convective boundary layer and this effect is even larger over the sea, where there is no diurnal variation of the height of the boundary layer as there is over land.[24] In the convective boundary layer, strong mixing diminishes vertical wind gradient.[25]
Implications
Engineering
The design of buildings must account for wind loads, and these are affected by wind gradient. The respective gradient levels, usually assumed in the Building Codes, are 500 meters for cities, 400 meters for suburbs, and 300 m for flat open terrain.[26] For engineering purposes, a power law wind speed profile may be defined as follows:[11][15]
- = wind speed at height
- = wind speed at gradient height
- = exponential coefficient
Wind turbines
Wind turbine operation is affected by wind gradient. Vertical wind-speed profiles result in different wind speeds at the blades nearest to the ground level compared to those at the top of blade travel, which results in asymmetric load.[27] The wind gradient can create a large bending moment in the shaft of a two-bladed turbine when the blades are vertical.[28] The reduced wind gradient over water means shorter and less expensive wind turbine towers can be used in windparks which are placed in (shallow) seas.[12] It would be preferable for wind turbines to be tested in a wind tunnel simulating the wind gradient that they will eventually see, but this is rarely done.[29]
For wind turbine engineering, a polynomial variation in wind speed with height can be defined relative to wind measured at a reference height of 10 meters as:[27]
- = velocity of the wind [m/s], at height
- = velocity of the wind [m/s], at height = 10 meters
- = Hellmann exponent
The Hellmann exponent depends upon the coastal location and the shape of the terrain on the ground, and the stability of the air. Examples of values of the Hellmann exponent are given in the table below:[30]
Location | a |
---|---|
Unstable air above open water surface | 0.06 |
Neutral air above open water surface | 0.10 |
Unstable air above flat open coast | 0.11 |
Neutral air above flat open coast | 0.16 |
Stable air above open water surface | 0.27 |
Unstable air above human inhabited areas | 0.27 |
Neutral air above human inhabited areas | 0.34 |
Stable air above flat open coast | 0.40 |
Stable air above human inhabited areas | 0.60 |
Gliding
In gliding, wind gradient affects the takeoff and landing phases of flight of a glider. Wind gradient can have a noticeable effect on
When landing, wind gradient is also a hazard, particularly when the winds are strong.[32] As the glider descends through the wind gradient on final approach to landing, airspeed decreases while sink rate increases, and there is insufficient time to accelerate prior to ground contact. The pilot must anticipate the wind gradient and use a higher approach speed to compensate for it.[33]
Wind gradient is also a hazard for aircraft making steep turns near the ground. It is a particular problem for gliders which have a relatively long
Sailing
In
The mast head instruments indication of apparent wind speed and direction is different from what the sailor sees and feels near the surface.
According to one source,[39] the wind gradient is not significant for sailboats when the wind is over 6 knots (because a wind speed of 10 knots at the surface corresponds to 15 knots at 300 meters, so the change in speed is negligible over the height of a sailboat's mast). According to the same source, the wind increases steadily with height up to about 10 meters in 5 knot winds but less if there is less wind. That source states that in winds with average speeds of six knots or more, the change of speed with height is confined almost entirely to the one or two meters closest to the surface.[40] This is consistent with another source, which shows that the change in wind speed is very small for heights over 2 meters[41] and with a statement by the Australian Government Bureau of Meteorology[42] according to which differences can be as little as 5% in unstable air.[43]
In
Sound propagation
Wind gradient can have a pronounced effect upon sound propagation in the lower atmosphere. This effect is important in understanding sound propagation from distant sources, such as
When the sun warms the Earth's surface, there is a negative temperature gradient in atmosphere. The speed of sound decreases with decreasing temperature, so this also creates a negative sound speed gradient.[48] The sound wave front travels faster near the ground, so the sound is refracted upward, away from listeners on the ground, creating an acoustic shadow at some distance from the source.[49] The radius of curvature of the sound path is inversely proportional to the velocity gradient.[50]
A wind speed gradient of 4 (m/s)/km can produce refraction equal to a typical temperature lapse rate of 7.5 °C/km.[51] Higher values of wind gradient will refract sound downward toward the surface in the downwind direction,[52] eliminating the acoustic shadow on the downwind side. This will increase the audibility of sounds downwind. This downwind refraction effect occurs because there is a wind gradient; the sound is not being carried along by the wind.[53]
There will usually be both a wind gradient and a temperature gradient. In that case, the effects of both might add together or subtract depending on the situation and the location of the observer.[54] The wind gradient and the temperature gradient can also have complex interactions. For example, a foghorn can be audible at a place near the source, and a distant place, but not in a sound shadow between them.[55] In the case of transverse sound propagation, wind gradients do not sensibly modify sound propagation relative to the windless condition; the gradient effect appears to be important only in upwind and downwind configurations.[56]
For sound propagation, the exponential variation of wind speed with height can be defined as follows:[46]
- = speed of the wind at height , and is a constant
- = exponential coefficient based on ground surface roughness, typically between 0.08 and 0.52
- = expected wind gradient at height
In the 1862 American Civil War Battle of Iuka, an acoustic shadow, believed to have been enhanced by a northeast wind, kept two divisions of Union soldiers out of the battle,[57] because they could not hear the sounds of battle only six miles downwind.[58]
Scientists have understood the effect of wind gradient upon refraction of sound since the mid-1900s; however, with the advent of the U.S. Noise Control Act, this refractive phenomenon was widely used beginning in the early 1970s, chiefly in the consideration of noise propagation from highways and resultant design of transportation facilities.[59]
Wind gradient soaring
Wind gradient soaring, also called
See also
References
- ^ ISBN 978-0-88385-709-0.
Thus we have a "wind-speed gradient" as we move vertically, and this has a tendency to encourage mixing between the air at one level and the air at those levels immediately above and below it.
- ^ Gorder, P.J.; Kaufman, K.; Greif, R. (1996). "Effect of wind gradient on the trajectory synthesis algorithms of the Center-TRACON Automation System (CTAS)". AIAA, Guidance, Navigation and Control Conference, San Diego, CA. American Institute of Aeronautics and Astronautics.
...the effect of a change in mean wind velocity with altitude, the wind velocity gradient...
[permanent dead link] - .
...the shear wind gradient is rather weak....the energy gain...is due to a mechanism other than the wind gradient effect.
- ^ ISBN 978-0-415-04319-9.
Therefore the vertical gradient of mean wind speed (dū/dz) is greatest over smooth terrain, and least over rough surfaces.
- ISBN 978-1-57958-201-2.
wind gradient = rate of increase of wind strength with unit increase in height above ground level;
- ^ ISBN 978-1-84407-262-0.
The relation between wind speed and height is called the wind profile or wind gradient.
- American Meteorological Association. Retrieved 2015-02-15.
- ^ ISBN 978-0-471-34877-1.
- ^ Dalgliesh, W. A. and D. W. Boyd (1962-04-01). "CBD-28. Wind on Buildings". Canadian Building Digest. Archived from the original on 2007-11-12. Retrieved 2007-06-07.
Flow near the surface encounters small obstacles that change the wind speed and introduce random vertical and horizontal velocity components at right angles to the main direction of flow.
- ^ ISBN 978-0-8493-5053-5.
- ^ ISBN 978-0-471-84298-9.
- ^ ISBN 978-3-540-40340-1.
- ISBN 978-0-85404-584-6.
- ^ ISBN 978-0-415-17145-8.
- ^ ISBN 978-0-8493-8969-6.
- ISBN 978-1-4020-2850-2.
- ISBN 978-0-8493-2674-5.
- ISBN 978-1-84265-125-4.
- ISBN 978-90-277-2768-8.
...both the wind gradient and the mean wind profile itself can usually be described diagnostically by the log wind profile.
- .
- ISBN 978-0-412-41160-1.
- ISBN 978-0-471-48997-9.
- .
- ^ Johansson, C.; Uppsala, S.; Smedman, A.S. (2002). "Does the height of the boundary layer influence the turbulence structure near the surface over the Baltic Sea?". 15th Conference on Boundary Layer and Turbulence. 15th Conference on Boundary Layer and Turbulence. American Meteorological Society.
- ISBN 978-0-7923-6657-7.
In the bulk of the convective boundary layer, strong mixing diminishes vertical wind gradient...
- ISBN 978-0-412-22230-6.
- ^ ISBN 978-0-470-86899-7.
- ISBN 978-0-471-49456-0.
- ISBN 978-0-471-55774-6.
It would be preferable to evaluate windmills in the wind gradient that they will eventually see, but this is rarely done.
- ^ "Renewable energy: technology, economics, and environment" by
Martin Kaltschmitt, Wolfgang Streicher, Andreas Wiese, (Springer, 2007, ISBN 978-3-540-70947-3), page 55
- ^ Glider Flying Handbook. U.S. Government Printing Office, Washington D.C.: U.S. Federal Aviation Administration. 2003. pp. 7–16. FAA-8083-13_GFH.
- ISBN 978-1-86126-414-5.
The reason for making the increase is because the wind speed increases with height (a `wind gradient')
- ^ ISBN 978-0-9605676-4-5.
The wind gradient is said to be steep or pronounced when the change in wind speed with height is very rapid, and it is in these conditions that extra care must be used when taking off or landing in a glider
- ISBN 978-0-9605676-3-8.
- ISBN 978-1-883813-02-4. If the pilot runs into the wind gradient as he is turning into the wind, there will obviously be less wind across the lower than the higher wing.
- ISBN 978-0-07-142381-6.
Wind shear is the difference in direction at varying heights above the water; wind gradient is the difference in wind strength at varying heights above the water.
- ISBN 978-0-312-04278-3.
You'll not recognize wind shear if your apparent wind angle is smaller on one tack than on the other because the apparent wind direction is a combination of boat speed and wind speed - and the sailing speed may be more determined by water conditions in one direction rather than another. This means that the faster a boat goes the more 'ahead' the apparent wind becomes. That is why the 'close reach' direction is the fastest direction of sailing – simply because as the boat speeds up the apparent wind direct goes further and further forward without stalling the sails and the apparent wind speed also increases – so increasing the boat's speed even further. This particular factor is exploited to the full in sand-yachting in which it is common for a sand yacht to exceed the wind speed as measured by a stationary observer. Wind shear is certainly felt because the wind speed at the masthead will be higher than at deck level. Thus gusts of wind can capsize a small sailing boat easily if the crew are not sufficiently wary.
- ^ ISBN 978-1-57409-000-0.
Wind speed and direction are normally measured at the top of the mast, and the wind gradient must therefore be known in order to determine the mean wind speed incident on the sail.
- ISBN 978-0-7136-6704-2. See sections 3.2 and 3.3.
- ^ See p. 11 of the cited book by Bethwaite
- ^ "Wind Gradient". Retrieved 2023-10-06.
- ^ "Wind Shear". Archived from the original on 2007-09-04. Retrieved 2023-10-06.
- ^ As explained in Bethwaite's book, the air is turbulent near the surface if the wind speed is greater than 6 knots
- ISBN 978-0-9542896-0-7.
- ^ Foss, Rene N. (June 1978). "Ground Plane Wind Shear Interaction on Acoustic Transmission". WA-RD 033.1. Washington State Department of Transportation. Retrieved 2007-05-30.
- ^ ISBN 978-0-415-26713-7.
As wind speed generally increases with altitude, wind blowing towards the listener from the source will refract sound waves downwards, resulting in increased noise levels.
- S2CID 109914430.
- ISBN 978-0-419-21810-4.
- ISBN 978-0-07-136097-5.
- Penn State University. pp. 10.6–10.7.
- ISBN 978-0-486-64575-9.
- ISBN 978-0-8493-8647-3.
- ISBN 978-1-84265-237-4.
It may be seen that refraction effects occur only because there is a wind gradient and it is not due to the result of sound being convected along by the wind.
- ^ N01-N07 Sound Ranging (PDF). Basic Science & Technology Section. Royal School Of Artillery. 2002-12-19. pp. N–12.
...there will usually be both a wind gradient and a temperature gradient.
- .
- Bibcode:1993ONERA....R....M.
- ISBN 978-1-56619-913-1.
- ISBN 978-0-8078-5783-0.
- ^ Hogan, C. Michael and Gary L. Latshaw, "The Relationship between Highway Planning and Urban Noise", Proceedings of the ASCE, Urban Transportation Division specialty conference, May 21/23, 1973, Chicago, Ill., American Society of Civil Engineers
- ISBN 978-0-691-08678-1.
- ISBN 978-0-521-44822-2.