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Wind is the Flux|flow of gas es on a large scale. On Earth , wind consists of the bulk movement of air. In outer space , solar wind is the movement of gases or charged particles from the sun through space, while planetary wind is the outgassing of light chemical element s from a planet's atmosphere into space. Winds are commonly classified by their scale (spatial)|spatial scale , their speed , the types of forces that cause them, the regions in which they occur, and their effect. The strongest observed winds on a planet in our solar system occur on Neptune and Saturn .

In meteorology , winds are often referred to according to their strength, and the direction from which the wind is blowing. Short bursts of high speed wind are termed gusts. Strong winds of intermediate duration (around one minute) are termed squall s. Long-duration winds have various names associated with their average strength, such as breeze, gale , Storm#Classification|storm , tropical cyclone|hurricane , and typhoon. Wind occurs on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to world|global winds resulting from the difference in absorption of solar energy between the climate zone s on Earth. The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet ( Coriolis effect ). Within the tropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations. In coastal areas the sea breeze /land breeze cycle can define local winds; in areas that have variable terrain, mountain and valley breezes can dominate local winds.

In human civilization , wind has inspired mythology , influenced the events of history , expanded the range of transport and warfare , and provided a wind power|power source for mechanical work , electricity and recreation . Wind powers the voyages of sailing ship s across Earth's oceans. Hot air balloon s use the wind to take short trips, and powered flight uses it to increase lift and reduce fuel consumption. Areas of wind shear caused by various weather phenomena can lead to dangerous situations for aircraft . When winds become strong, trees and man-made structures are damaged or destroyed.

Winds can shape landforms, via a variety of aeolian processes such as the formation of fertile soils, such as loess , and by erosion . Dust from large desert s can be moved great distances from its source region by the prevailing winds ; winds that are accelerated by rough topography and associated with dust outbreaks have been assigned regional names in various parts of the world because of their significant effects on those regions. Wind affects the spread of wildfire s. Winds disperse seeds from various plants, enabling the survival and dispersal of those plant species, as well as flying insect populations. When combined with cold temperatures, wind has a negative impact on livestock . Wind affects animals' food stores, as well as their hunting and defensive strategies.

Cause

Wind is caused by differences in pressure. When a pressure gradient force|difference in pressure exists, the air is accelerated from higher to lower pressure. On a rotating planet, the air will be deflected by the Coriolis effect , except exactly on the equator. Globally, the two major driving factors of large-scale winds (the atmospheric circulation ) are the differential heating between the equator and the poles (difference in absorption of solar energy leading to buoyancy force s) and the Coriolis effect|rotation of the planet . Outside the tropics and aloft from frictional effects of the surface, the large-scale winds tend to approach geostrophic balance . Near the Earth's surface, friction causes the wind to be slower than it would be otherwise. Surface friction also causes winds to blow more inward into low pressure areas.

Winds defined by an equilibrium of physical forces are used in the decomposition and analysis of wind profiles. They are useful for simplifying the atmospheric equations of motion and for making qualitative arguments about the horizontal and vertical distribution of winds. The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force. It flows parallel to isobar (meteorology)|isobars and approximates the flow above the atmospheric boundary layer in the midlatitudes. The thermal wind is the difference in the geostrophic wind between two levels in the atmosphere. It exists only in an atmosphere with horizontal temperature gradient s. The ageostrophy|ageostrophic wind component is the difference between actual and geostrophic wind, which is responsible for air "filling up" cyclones over time. The gradient wind is similar to the geostrophic wind but also includes centrifugal force (or centripetal acceleration ).

Measurement

Wind direction is reported by the direction from which it originates. For example, a northerly wind blows from the north to the south. Weather vane s pivot to indicate the direction of the wind. At airports, windsock s are primarily used to indicate wind direction, but can also be used to estimate wind speed by its angle of hang. Wind speed is measured by anemometer s, most commonly using rotating cups or propellers. When a high measurement frequency is needed (such as in research applications), wind can be measured by the propagation speed of ultrasound signals or by the effect of ventilation on the resistance of a heated wire. Another type of anemometer uses pitot tube s that take advantage of the pressure differential between an inner tube and an outer tube that is exposed to the wind to determine the dynamic pressure, which is then used to compute the wind speed.

Sustained wind speeds are reported globally at a height and are averaged over a 10& nbsp;minute time frame. The United States reports winds over a 1& nbsp;minute average for tropical cyclones, and a 2& nbsp;minute average within weather observations.Office of the Federal Coordinator for Meteorology. Retrieved on 2008-04-06. India typically reports winds over a 3& nbsp;minute average. Knowing the wind sampling average is important, as the value of a one-minute sustained wind is typically 14% greater than a ten-minute sustained wind. A short burst of high speed wind is termed a wind gust, one technical definition of a wind gust is: the maxima that exceed the lowest wind speed measured during a ten minute time interval by . A squall is a doubling of the wind speed above a certain threshold, which lasts for a minute or more.

To determine winds aloft, rawinsondes determine wind speed by GPS , LORAN|radio navigation , or radar tracking of the probe. Alternatively, movement of the parent weather balloon position can be tracked from the ground visually using theodolite s. Remote sensing techniques for wind include SODAR , Doppler effect|Doppler LIDAR s and RADAR s, which can measure the Doppler shift of electromagnetic radiation scattered or reflected off suspended aerosol s or molecule s, and radiometer s and radars can be used to measure the surface roughness of the ocean from space or airplanes. Ocean roughness can be used to estimate wind velocity close to the sea surface over oceans. Geostationary satellite imagery can be used to estimate the winds throughout the atmosphere based upon how far clouds move from one image to the next. Wind Engineering describes the study of the effects of the wind on the built environment, including buildings, bridges and other man-made objects.

Wind force scale

Historically, the Beaufort scale|Beaufort wind force scale provides an empirical description of wind speed based on observed sea conditions. Originally it was a 13-level scale, but during the 1940s, the scale was expanded to 17& nbsp;levels. There are general terms that differentiate winds of different average speeds such as a breeze, a gale, a storm, tornado, or a hurricane. Within the Beaufort scale, gale-force winds lie between and with preceding adjectives such as moderate, fresh, strong, and whole used to differentiate the wind's strength within the gale category. A storm has winds of to . The terminology for tropical cyclones differs from one region to another globally. Most ocean basins use the average wind speed to determine the tropical cyclone's category. Below is a summary of the classifications used by Regional Specialized Meteorological Centre|Regional Specialized Meteorological Centers worldwide:

General wind classifications			Tropical cyclone classifications (all winds are 10-minute averages)
Beaufort scale	knots )	cite web>year=2009	Indian Meteorological Department>IMD	Météo-France>MF	South Pacific Bureau of Meteorology (Australia)>BMKG , Fiji Meteorological Service	Japan Meteorological Agency>JMA	Joint Typhoon Warning Center>JTWC	N Atlantic National Hurricane Center>CPHC
0	<1	Calm	Low Pressure Area	Tropical disturbance	Tropical low Tropical Depression	Tropical depression	Tropical depression	Tropical depression
1	1–3	Light air
2	4–6	Light breeze
3	7–10	Gentle breeze
4	11–16	Moderate breeze
5	17–21	Fresh breeze	Depression
6	22–27	Strong breeze	Depression
7	28–29	Moderate gale	Deep depression	Tropical depression
7	30–33	Moderate gale	Deep depression	Tropical depression
8	34–40	Fresh gale	Cyclonic storm	Moderate tropical storm	Tropical cyclone (1)	Tropical storm	Tropical storm	Tropical storm
9	41–47	Strong gale	Cyclonic storm	Moderate tropical storm	Tropical cyclone (1)	Tropical storm
10	48–55	Whole gale	Severe cyclonic storm	Severe tropical storm	Tropical cyclone (2)	Severe tropical storm
11	56–63	Storm	Severe cyclonic storm	Severe tropical storm	Tropical cyclone (2)	Severe tropical storm
12	64–72	Hurricane	Very severe cyclonic storm	Tropical cyclone	Severe tropical cyclone (3)	Typhoon	Typhoon	Hurricane (1)
13	73–85				Severe tropical cyclone (3)			Hurricane (2)
14	86–89				Severe tropical cyclone (4)			Major hurricane (3)
15	90–99			Intense tropical cyclone				Major hurricane (3)
16	100–106							Major hurricane (4)
17	107–114				Severe tropical cyclone (5)
	115–119			Very intense tropical cyclone			Super typhoon
	>120		Super cyclonic storm	Very intense tropical cyclone			Super typhoon	Major hurricane (5)

Fujita scale

The Enhanced Fujita Scale (EF Scale) rates the strength of tornadoes in the United States based on the damage they cause. Below is that scale.

Scale	Wind speed		Relative frequency	Potential damage
	mph	km/ h
65–85	Minor or no damage.Peels surface off some roofs; some damage to gutters or siding; branches broken off trees; shallow-rooted trees pushed over.Confirmed tornadoes with no reported damage (i.e., those that remain in open fields) are always rated EF0.
86–110 Roofs severely stripped; mobile homes overturned or badly damaged; loss of exterior doors; windows and other glass broken.
111–135 Roofs torn off well-constructed houses; foundations of frame homes shifted; mobile homes completely destroyed; large trees snapped or uprooted; light-object missiles generated; cars lifted off ground.
136–165 Entire stories of well-constructed houses destroyed; severe damage to large buildings such as shopping malls; trains overturned; trees debarked; heavy cars lifted off the ground and thrown; structures with weak foundations are badly damaged.
166–200 Well-constructed and whole frame houses completely leveled; cars and other large objects thrown and small missiles generated.
>200 Strong-framed, well-built houses leveled off and foundations swept away; steel-reinforced concrete structures are critically damaged; tall buildings collapse or have severe structural deformations.

Station model

The station model plotted on surface weather map s uses a wind barb to show both wind direction and speed. The wind barb shows the speed using "flags" on the end.

Each half of a flag depicts of wind.

Each full flag depicts of wind.

Each pennant (commissioning)|pennant (filled triangle) depicts of wind.

Winds are depicted as blowing from the direction the barb is facing. Therefore, a northeast wind will be depicted with a line extending from the cloud circle to the northeast, with flags indicating wind speed on the northeast end of this line. Once plotted on a map, an analysis of isotach s (lines of equal wind speeds) can be accomplished. Isotachs are particularly useful in diagnosing the location of the jet stream on upper level constant pressure charts, and are usually located at or above the 300& nbsp;hPa level.

Wind energy

Wind energy is the kinetic energy of the air in motion. Total wind energy flowing through an imaginary area A during the time t is:

:E = A·v·t·?·½ v²,

where v is the wind velocity and ? is the air density . The formula presented is structured in two parts: (A·v·t) is the volume of air passing through A, which is considered perpendicular to the wind velocity; (?·½ v²) is the kinetic energy of the moving air per unit volume.

Total wind power is:

:P = E/t = A·?·½ v³

Wind power is thus proportional to the third power of the wind velocity.

Theoretical power captured by a wind turbine

Total wind power could be captured only if the wind velocity is reduced to zero. In a realistic wind turbine this is impossible, as the captured air must also leave the turbine. A relation between the input and output wind velocity must be considered. Using the concept of stream tube , the maximal achievable extraction of wind power by a wind turbine is 59% of the total theoretical wind power. Kira Grogg Carleton College (2005) p. 8. (PDF). Retrieved on 2011-11-03. (see: Betz' law ).

Practical wind turbine power

Further insufficiencies, such as rotor blade friction and drag (physics)|drag , gearbox losses, generator and converter losses, reduce the power delivered by a wind turbine. The basic relation that the turbine power is (approximately) proportional to the third power of velocity remains.

Global climatology

Easterly winds, on average, dominate the flow pattern across the poles, westerly winds blow across the mid-latitudes of the earth, to the north of the subtropical ridge , while easterlies again dominate the tropics .

Directly under the subtropical ridge are the doldrums, or horse latitudes, where winds are lighter. Many of the Earth's deserts lie near the average latitude of the subtropical ridge, where descent reduces the relative humidity of the air mass. The strongest winds are in the mid-latitudes where cold Arctic air meets warm air from the tropics.

Tropics

The trade winds (also called trades) are the prevailing pattern of easterlies|easterly surface winds found in the tropics towards the Earth's equator . The trade winds blow predominantly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere . The trade winds act as the Tropical cyclone#Steering wind|steering flow for tropical cyclones that form over world's oceans. Trade winds also steer African dust westward across the Atlantic Ocean into the Caribbean Sea , as well as portions of southeast North America .

A monsoon is a seasonal prevailing wind that lasts for several months within tropical regions. The term was first used in English in India , Bangladesh , Pakistan , and neighboring countries to refer to the big seasonal winds blowing from the Indian Ocean and Arabian Sea in the southwest bringing heavy rainfall to the area. Its poleward progression is accelerated by the development off a heat low over the Asian, African, and North American continents during May through July, and over Australia in December.

Westerlies and their impact

The Westerlies or the Prevailing Westerlies are the prevailing winds in the middle latitudes between 35 and 65& nbsp;degrees latitude . These prevailing winds blow from the west to the east to the north of the subtropical ridge, and steer extratropical cyclones in this general manner. The winds are predominantly from the southwest in the Northern Hemisphere and from the northwest in the Southern Hemisphere . They are strongest in the winter when the pressure is lower over the poles, and weakest during the summer and when pressures are higher over the poles.

Together with the trade wind s, the westerlies enabled a round-trip trade route for sailing ships crossing the Atlantic and Pacific Oceans, as the westerlies lead to the development of strong ocean currents on the western sides of oceans in both hemispheres through the process of western intensification. These western ocean currents transport warm, sub tropical water polewards toward the polar region s. The westerlies can be particularly strong, especially in the southern hemisphere, where there is less land in the middle latitudes to cause the flow pattern to amplify, which slows the winds down. The strongest westerly winds in the middle latitudes are within a band known as the Roaring Forties , between 40th parallel south|40 and 50th parallel south|50& nbsp;degrees latitude south of the equator. The Westerlies play an important role in carrying the warm, equatorial waters and winds to the western coasts of continents, especially in the southern hemisphere because of its vast oceanic expanse.

Polar easterlies

The polar easterlies, also known as Polar Hadley cells, are dry, cold prevailing winds that blow from the high-pressure areas of the polar high s at the north pole|north and south pole s towards the low-pressure areas within the Westerlies at high latitudes. Unlike the Westerlies, these prevailing winds blow from the east to the west , and are often weak and irregular. Because of the low sun angle, cold air builds up and Subsidence (atmosphere)|subsides at the pole creating surface high-pressure areas, forcing an equatorward outflow of air; that outflow is deflected eastward by the Coriolis effect.

Local considerations

Sea and land breezes

In coastal regions, sea breezes and land breezes can be important factors in a location's prevailing winds. The ocean|sea is warmed by the sun more slowly because of water's greater specific heat compared to land. As the temperature of the surface of the landform|land rises, the land heats the air above it by conduction. The warm air is less dense than the surrounding environment and so it rises. This causes a pressure gradient of about 2& nbsp;millibars from the ocean to the land. The cooler air above the sea, now with higher sea level pressure , flows inland into the lower pressure, creating a cooler breeze near the coast. When large-scale winds are calm, the strength of the sea breeze is directly proportional to the temperature difference between the land mass and the sea. If an offshore wind of exists, the sea breeze is not likely to develop.

At night, the land cools off more quickly than the ocean because of differences in their specific heat values. This temperature change causes the daytime sea breeze to dissipate. When the temperature onshore cools below the temperature offshore, the pressure over the water will be lower than that of the land, establishing a land breeze, as long as an onshore wind is not strong enough to oppose it.

Near mountains

Over elevated surfaces, heating of the ground exceeds the heating of the surrounding air at the same altitude above sea level , creating an associated thermal low over the terrain and enhancing any thermal lows that would have otherwise existed, and changing the wind circulation of the region. In areas where there is rugged topography that significantly interrupts the environmental wind flow, the wind circulation between mountains and valleys is the most important contributor to the prevailing winds. Hills and valleys substantially distort the airflow by increasing friction between the atmosphere and landmass by acting as a physical block to the flow, deflecting the wind parallel to the range just upstream of the topography, which is known as a barrier jet . This barrier jet can increase the low level wind by 45%. Wind direction also changes because of the contour of the land.

If there is a mountain pass|pass in the mountain range, winds will rush through the pass with considerable speed because of the Bernoulli principle that describes an inverse relationship between speed and pressure. The airflow can remain turbulent and erratic for some distance downwind into the flatter countryside. These conditions are dangerous to ascending and descending airplane s. Cool winds accelerating through mountain gaps have been given regional names. In Central America , examples include the Papagayo wind , the Panama wind, and the Tehuano wind . In Europe , similar winds are known as the Bora (wind)|Bora , Tramontane , and Mistral (wind)|Mistral . When these winds blow over open waters, they increase mixing of the upper layers of the ocean that elevates cool, nutrient rich waters to the surface, which leads to increased marine life.

In mountainous areas, local distortion of the airflow becomes severe. Jagged terrain combines to produce unpredictable flow patterns and turbulence, such as lee waves|rotors , which can be topped by lenticular cloud s. Strong updraft s, downdrafts and eddies develop as the air flows over hills and down valleys. Orographic precipitation (meteorology)|precipitation occurs on the windward side of mountains and is caused by the rising air motion of a large-scale flow of moist air across the mountain ridge, also known as upslope flow, resulting in adiabatic lapse rate|adiabatic cooling and condensation. In mountainous parts of the world subjected to relatively consistent winds (for example, the trade winds), a more moist climate usually prevails on the windward side of a mountain than on the leeward or downwind side. Moisture is removed by orographic lift, leaving drier air on the descending and generally warming, leeward side where a rain shadow is observed. Winds that flow over mountains down into lower elevations are known as downslope winds. These winds are warm and dry. In Europe downwind of the Alps , they are known as foehn . In Poland , an example is the halny wiatr. In Argentina, the local name for downsloped winds is zonda (wind)|zonda . In Java, the local name for such winds is koembang. In New Zealand , they are known as the Nor'west arch , and are accompanied by the cloud formation they are named after that has inspired artwork over the years. In the Great Plains of the United States, the winds are known as a chinook wind|chinook . In California, downsloped winds are funneled through mountain passes, which intensify their effect, and examples into Santa Ana wind|Santa Ana and sundowner (wind)|sundowner winds. Wind speeds during downslope wind effect can exceed .

Average wind speeds

As described earlier, prevailing and local winds are not spread evenly across the earth, which means that wind speeds also differ by region. In addition, the wind speed also increases with the altitude.

Wind power density

Nowadays, a yardstick used to determine the best locations for wind energy development is referred to as wind power density (WPD). It is a calculation relating to the effective force of the wind at a particular location, frequently expressed in terms of the elevation above ground level over a period of time. It takes into account wind velocity and mass. Color coded maps are prepared for a particular area are described as, for example, "mean annual power density at 50& nbsp;meters." The results of the above calculation are included in an index developed by the National Renewable Energy Lab and referred to as "NREL CLASS." The larger the WPD calculation, the higher it is rated by class.Kansas Wind Energy Project, Affiliated Atlantic & Western Group Inc, 5250 W 94th Terrace, Prairie Village, Kansas 66207 At the end of 2008, worldwide nameplate capacity of wind-powered generators was 120.8& nbsp; gigawatt s. Although wind produces only about 1.5% of worldwide electricity use, it is growing rapidly, having doubled in the three years between 2005 and 2008. In several countries it has achieved relatively high levels of penetration, accounting for approximately 19% of electricity production in Wind power in Denmark|Denmark , 10% in Wind power in Spain|Spain and Wind power in Portugal|Portugal , and 7% in Wind power in Germany|Germany and the Wind power in Ireland|Republic of Ireland in 2008. One study indicates that an entirely renewable energy supply based on 70% wind is attainable at today's power prices by linking wind farm s with an High-voltage direct current|HVDC supergrid.

Shear

Wind shear, sometimes referred to as windshear or wind gradient , is a difference in wind speed and direction over a relatively short distance in the Earth's atmosphere. Wind shear can be broken down into vertical and horizontal components, with horizontal wind shear seen across weather fronts and near the coast, and vertical shear typically near the surface, though also at higher levels in the atmosphere near upper level jets and frontal zones aloft.

Wind shear itself is a microscale meteorology|microscale meteorological phenomenon occurring over a very small distance, but it can be associated with mesoscale meteorology|mesoscale or synoptic scale weather features such as squall line s and cold front s. It is commonly observed near microburst s and downburst s caused by thunderstorm s, weather fronts, areas of locally higher low level winds referred to as low level jets, near mountain s, radiation inversions that occur because of clear skies and calm winds, buildings, wind turbine s, and sailboat s. Wind shear has a significant effect during take-off and landing of aircraft because of their effects on control of the aircraft, and was a significant cause of aircraft accidents involving large loss of life within the United States .

Sound movement through the atmosphere is affected by wind shear, which can bend the wave front, causing sounds to be heard where they normally would not, or vice versa. Strong vertical wind shear within the troposphere also inhibits tropical cyclone development, but helps to organize individual thunderstorms into living longer life cycles that can then produce severe weather . The thermal wind concept explains how differences in wind speed with height are dependent on horizontal temperature differences, and explains the existence of the jet stream.

Usage of wind

History

As a natural force, the wind was often personified as one or more wind god s or as an expression of the supernatural in many cultures. Vayu is the Hindu God of Wind. The Greek wind gods include Boreas (god)|Boreas , Greek Goddess|Notus , Eurus , and Zephyrus . Aeolus , in varying interpretations the ruler or keeper of the four winds, has also been described as Astraeus , the god of dusk who fathered the four winds with Eos , goddess of dawn. The Ancient Greeks also observed the seasonal change of the winds, as evidenced by the Tower of the Winds in Athens . Venti are the Roman gods of the winds. Fujin , the Japanese wind god and is one of the eldest Shinto gods. According to legend, he was present at the creation of the world and first let the winds out of his bag to clear the world of mist. In Norse mythology , Njord is the god of the wind. There are also four dvärgar ( Norse dwarves ), named Norðri, Suðri, Austri and Vestri , and probably the four stags of Yggdrasil , personify the four winds, and parallel the four Greek wind gods. Stribog is the name of the Slavic Mythology|Slavic god of winds, sky and air. He is said to be the ancestor (grandfather) of the winds of the eight directions.

Kamikaze (typhoon)|Kamikaze (??) is a Japanese word, usually translated as divine wind, believed to be a gift from the gods. The term is first known to have been used as the name of a pair or series of typhoons that are said to have saved Japan from two Mongol fleets under Kublai Khan that attacked Japan in 1274 and again in 1281. Protestant Wind is a name for the storm that deterred the Spanish Armada from an invasion of England in 1588 where the wind played a pivotal role, or the favorable winds that enabled William III of England|William of Orange to invade England in 1688. During Napoleon I of France|Napoleon 's French Invasion of Egypt (1798)|Egyptian Campaign , the French soldiers had a hard time with the khamsin wind: when the storm appeared "as a blood-stint in the distant sky", the natives went to take cover, while the French "did not react until it was too late, then choked and fainted in the blinding, suffocating walls of dust." During the North African Campaign of the World War II , "allied and German troops were several times forced to halt in mid-battle because of sandstorms caused by khamsin ... Grains of sand whirled by the wind blinded the soldiers and created electrical disturbances that rendered compasses useless."

Transportation

There are many different forms of sailing ships, but they all have certain basic things in common. Except for rotor ship s using the Magnus effect , every sailing ship has a hull (ship)|hull , rigging and at least one mast (sailing)|mast to hold up the sail s that use the wind to power the ship. Ocean journeys by sailing ship can take many months, and a common hazard is becoming becalmed because of lack of wind, or being blown off course by severe storm s or winds that do not allow progress in the desired direction. A severe storm could lead to shipwreck , and the loss of all hands. Sailing ships can only carry a certain quantity of supplies in their hold (ship)|hold , so they have to plan long Maritime history|voyages carefully to include appropriate Provisioning of the USS Constitution|provisions , including fresh water .

For aerodynamic aircraft which operate relative to the air, winds affect groundspeed, and in the case of lighter-than-air vehicles, wind may play a significant or solitary role in their movement and ground track. The velocity of surface wind is generally the primary factor governing the direction of flight operations at an airport, and airfield runways are aligned to account for the common wind direction(s) of the local area. While taking off with a tailwind may be necessary under certain circumstances, a headwind is generally desirable. A tailwind increases takeoff distance required and decreases the climb gradient.

Power source

Historically, the ancient Sinhala people|Sinhalese of Anuradhapura and in other cities around Sri Lanka used the monsoon winds to power furnaces as early as 300 Common Era|BCE . The furnaces were constructed on the path of the monsoon winds to exploit the wind power, to bring the temperatures inside up to . An early historical reference to a rudimentary windmill was used to power an organ (music)|organ in the first century CE. The first practical windmill s were later built in Sistan , Afghanistan , from the 7th century CE. These were vertical-axle windmills, which had long vertical driveshaft s with rectangle shaped blades. Made of six to twelve Windmill sail|sails covered in reed mat (craft)|reed matting or cloth material, these windmills were used to grind corn and draw up water, and were used in the gristmill ing and sugarcane industries. Horizontal-axle windmills were later used extensively in Northwestern Europe to grind flour beginning in the 1180s, and many Dutch windmills still exist. is the focus of over 30 companies worldwide using tethered technology rather than ground-hugging compressive-towers. Oil is being saved by using wind for powering cargo ships by use of the mechanical energy converted from the wind's kinetic energy using very large kites.. SkySails.. Retrieved on 2011-11-03.

Recreation

Wind figures prominently in several popular sports, including recreational hang gliding , hot air ballooning , kite|kite flying , snowkiting , kite landboarding , kite surfing , paragliding , sailing , and windsurfing . In gliding, wind gradients just above the surface affect the takeoff and landing phases of flight of a Glider aircraft|glider . Wind gradient can have a noticeable effect on ground launch es, also known as winch launches or wire launches. If the wind gradient is significant or sudden, or both, and the pilot maintains the same pitch attitude, the indicated airspeed will increase, possibly exceeding the maximum ground launch tow speed. The pilot must adjust the airspeed to deal with the effect of the gradient. When landing, wind shear is also a hazard, particularly when the winds are strong. 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.

Role in the natural world

In arid climates, the main source of erosion is wind. The general wind circulation moves small particulates such as dust across wide oceans thousands of kilometers downwind of their point of origin, which is known as deflation. Westerly winds in the mid-latitudes of the planet drive the movement of ocean currents from west to east across the world's oceans. Wind has a very important role in aiding plants and other immobile organisms in dispersal of seeds, spores, pollen, etc. Although wind is not the primary form of seed dispersal in plants, it provides dispersal for a large percentage of the biomass of land plants.

Erosion

Erosion can be the result of material movement by the wind. There are two main effects. First, wind causes small particles to be lifted and therefore moved to another region. This is called deflation. Second, these suspended particles may impact on solid objects causing erosion by abrasion (ecological succession). Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation. An example is the formation of sand dunes , on a beach or in a desert. Loess is a homogeneous, typically nonstratified, porous, friable , slightly coherent, often calcareous, fine-grained, silt y, pale yellow or buff, windblown (Aeolian) sediment . It generally occurs as a widespread blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick. Loess often stands in either steep or vertical faces. Loess tends to develop into highly rich soils. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world. Loess deposits are geologically unstable by nature, and will erode very readily. Therefore, windbreaks (such as big trees and bushes) are often planted by farmers to reduce the wind erosion of loess.

Desert dust migration

During mid-summer (July), the westward-moving trade winds south of the northward-moving subtropical ridge expand northwestward from the Caribbean Sea into southeastern North America. When dust from the Sahara moving around the southern periphery of the ridge within the belt of trade winds moves over land, rainfall is suppressed and the sky changes from a blue to a white appearance, which leads to an increase in red sunsets. Its presence negatively impacts air quality by adding to the count of airborne particulates. Over 50% of the African dust that reaches the United States affects Florida. Since 1970, dust outbreaks have worsened because of periods of drought in Africa. There is a large variability in the dust transport to the Caribbean and Florida from year to year. Dust events have been linked to a decline in the health of coral reef s across the Caribbean and Florida, primarily since the 1970s. Similar dust plumes originate in the Gobi desert , which combined with pollutants, spread large distances downwind, or eastward, into North America.

There are local names for winds associated with sand and dust storms. The Calima carries dust on southeast winds into the Canary islands . The Harmattan carries dust during the winter into the Gulf of Guinea . The Sirocco brings dust from north Africa into southern Europe because of the movement of extratropical cyclones through the Mediterranean Sea . Spring storm systems moving across the eastern Mediterranean Sea cause dust to carry across Egypt and the Arabian peninsula , which are locally known as Khamsin . The Shamal (wind)|Shamal is caused by cold fronts lifting dust into the atmosphere for days at a time across the Persian Gulf states.

Effect on plants

Wind dispersal of seeds, or anemochory , is one of the more primitive means of dispersal. Wind dispersal can take on one of two primary forms: seeds can float on the breeze or alternatively, they can flutter to the ground. The classic examples of these dispersal mechanisms include dandelion s ( Taraxacum spp., Asteraceae ), which have a feathery pappus (flower structure)|pappus attached to their seeds and can be dispersed long distances, and maple s ( Acer (genus) spp., Sapindaceae ), which have winged seeds and flutter to the ground. An important constraint on wind dispersal is the need for abundant seed production to maximize the likelihood of a seed landing in a site suitable for germination . There are also strong evolutionary constraints on this dispersal mechanism. For instance, species in the Asteraceae on island s tended to have reduced dispersal capabilities (i.e., larger seed mass and smaller pappus) relative to the same species on the mainland. Reliance upon wind dispersal is common among many weed y or ruderal species. Unusual mechanisms of wind dispersal include tumbleweed s. A related process to anemochory is anemophily , which is the process where pollen is distributed by wind. Large families of plants are pollinated in this manner, which is favored when individuals of the dominant plant species are spaced closely together.

Wind also limits tree growth. On coast s and isolated mountains, the tree line is often much lower than in corresponding altitudes inland and in larger, more complex mountain systems, because strong winds reduce tree growth. High winds scour away thin soil s through erosion, as well as damage limbs and twigs. When high winds knock down or uproot trees, the process is known as windthrow . This is most likely on windward slopes of mountains, with severe cases generally occurring to tree stand s that are 75& nbsp;years or older. Plant varieties near the coast, such as the Sitka spruce and Coccoloba uvifera|sea grape , are pruning|pruned back by wind and salt spray near the coastline.

Wind can also cause plants damage through sand abrasion . Strong winds will pick up loose sand and topsoil and hurl it through the air at speeds ranging from 25–40 miles per hour. Such windblown sand causes extensive damage to plant seedlings because it ruptures plant cells, making them vulnerable to evaporation and drought. Using a mechanical sandblaster in a laboratory setting, scientists affiliated with the Agricultural Research Service studied the effects of windblown sand abrasion on cotton seedlings. The study showed that the seedlings responded to the damage created by the windblown sand abrasion by shifting energy from stem and root growth to the growth and repair of the damaged stems.. Ars.usda.gov. Retrieved on 2011-11-03. After a period of four weeks the growth of the seedling once again became uniform throughout the plant, as it was before the windblown sand abrasion occurred.

Effect on animals

Cattle and sheep are prone to wind chill caused by a combination of wind and cold temperatures, when winds exceed , rendering their hair and wool coverings ineffective. Although penguin s use both a layer of fat and feather s to help guard against coldness in both water and air, their flipper (anatomy)|flippers and feet are less immune to the cold. In the coldest climates such as Antarctica , emperor penguin s use huddle|huddling behavior to survive the wind and cold, continuously alternating the members on the outside of the assembled group, which reduces heat loss by 50%. Flying insect s, a subset of arthropods , are swept along by the prevailing winds, while birds follow their own course taking advantage of wind conditions, in order to either fly or glide. As such, fine line patterns within weather radar imagery, associated with converging winds, are dominated by insect returns. Bird migration, which tends to occur overnight within the lowest of the Earth's atmosphere , contaminates wind profiles gathered by weather radar, particularly the WSR-88D , by increasing the environmental wind returns by to .

Pika s use a wall of pebbles to store dry plants and grasses for the winter in order to protect the food from being blown away. Cockroach es use slight winds that precede the attacks of potential predator s, such as toad s, to survive their encounters. Their cercus|cerci are very sensitive to the wind, and help them survive half of their attacks. Elk has a keen sense of smell that can detect potential upwind predators at a distance of . Increases in wind above signals glaucous gull s to increase their foraging and aerial attacks on thick-billed murres .

Related damage

High winds are known to cause damage, depending upon their strength. Infrequent wind gusts can cause poorly designed suspension bridge s to sway. When wind gusts are at a similar frequency to the swaying of the bridge, the bridge can be destroyed more easily, such as what occurred with the Tacoma Narrows Bridge (1940)|Tacoma Narrows Bridge in 1940. Wind speeds as low as can lead to power outages due to tree branches disrupting the flow of energy through power lines. While no species of tree is guaranteed to stand up to hurricane-force winds, those with shallow roots are more prone to uproot, and brittle trees such as eucalyptus , sea hibiscus , and avocado are more prone to damage. Hurricane-force winds cause substantial damage to mobile homes, and begin to structurally damage homes with foundations. Winds of this strength due to downsloped winds off terrain have been known to shatter windows and sandblast paint from cars. Once winds exceed , homes completely collapse, and significant damage is done to larger buildings. Total destruction to man-made structures occurs when winds reach . The Saffir-Simpson scale and Enhanced Fujita scale were designed to help estimate wind speed from the damage caused by high winds related to tropical cyclones and tornado es, and vice versa.

Australia's Barrow Island (Western Australia)|Barrow Island holds the record for the strongest wind gust, reaching 408& nbsp;km/h (253& nbsp;mph) during tropical cyclone Olivia on 10 April 1996, surpassing the previous record of 372& nbsp;km/h (231& nbsp;mph) set on Mount Washington (New Hampshire) on the afternoon of 12 April 1934. The most powerful gusts of wind on Earth were created by nuclear detonations. The blast wave is similar to a strong wind gust over the ground. The largest nuclear explosion (50–58 megatons at an altitude of about 13,000& nbsp;ft) generated a 20 bar blast pressure at ground zero, which is similar to a wind gust of 3,100 miles per hour.

Wildfire intensity increases during daytime hours. For example, burn rates of smoldering logs are up to five times greater during the day because of lower humidity, increased temperatures, and increased wind speeds. Sunlight warms the ground during the day and causes air currents to travel uphill, and downhill during the night as the land cools. Wildfires are fanned by these winds and often follow the air currents over hills and through valleys. United States wildfire operations revolve around a 24-hour fire day that begins at 10:00& nbsp;a.m. because of the predictable increase in intensity resulting from the daytime warmth.

In outer space

The solar wind is quite different from a terrestrial wind, in that its origin is the sun, and it is composed of charged particles that have escaped the sun's atmosphere. Similar to the solar wind, the planetary wind is composed of light gases that escape planetary atmospheres. Over long periods of time, the planetary wind can radically change the composition of planetary atmospheres.

Planetary wind

The hydrodynamic wind within the upper portion of a planet's atmosphere allows light chemical elements such as hydrogen to move up to the exobase , the lower limit of the exosphere , where the gases can then reach escape velocity , entering outer space without impacting other particles of gas. This type of gas loss from a planet into space is known as planetary wind. Such a process over geologic time causes water-rich planets such as the Earth to evolve into planets like Venus . Additionally, planets with hotter lower atmospheres could accelerate the loss rate of hydrogen.

Solar wind

Rather than air, the solar wind is a Electric current|stream of charged particles —a plasma (physics)|plasma —ejected from the stellar atmosphere|upper atmosphere of the sun at a rate of . It consists mostly of electrons and proton s with energies of about 1 electron volt|keV . The stream of particles varies in temperature and speed with the passage of time. These particles are able to escape the sun's gravity , in part because of the high temperature of the corona , but also because of high kinetic energy that particles gain through a process that is not well-understood. The solar wind creates the Heliosphere , a vast bubble in the interstellar medium surrounding the solar system. Planets require large magnetic fields in order to reduce the ionization of their upper atmosphere by the solar wind. Other phenomena include geomagnetic storm s that can knock out power grids on Earth, the aurora (phenomenon)|aurorae such as the Aurora (astronomy)|Northern Lights , and the plasma tails of comet s that always point away from the sun.

On other planets

Strong winds at Venus's cloud tops circle the planet every four to five earth days. When the poles of Mars are exposed to sunlight after their winter , the frozen CO₂ Sublimation (physics)|sublimes , creating significant winds that sweep off the poles as fast as , which subsequently transports large amounts of dust and water vapor over its landscape . Other Martian winds have resulted in cleaning event s and Spirit rover#Dust devils|dust devils .. Nasa.gov. Retrieved on 2011-11-03. On Jupiter , wind speeds of are common in zonal jet streams. Saturn's winds are among the solar system's fastest. Cassini–Huygens data indicated peak easterly winds of . On Uranus , northern hemisphere wind speeds reach as high as near 50& nbsp;degrees north latitude. At the cloud tops of Neptune , prevailing winds range in speed from along the equator to at the poles. At 70° S latitude on Neptune, a high-speed jet stream travels at a speed of .

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