An anemometer is a device for measuring the velocity or the pressure of the wind, and is one instrument used in a weather station. The term is derived from the Greek word "anemos" meaning wind. Wind speed is the speed of movement of air relative to a fixed point on the earth. ... The use of water pressure - the Captain Cook Memorial Jet in Lake Burley Griffin, Canberra. ... Wind is the roughly horizontal movement of air (as opposed to an air current) caused by uneven heating of the Earths surface. ... A technician checks data from a weather station. ...

Anemometers may be divided into two classes: those that measure the velocity of the wind, and those that measure the pressure of the wind, but as there is a close connection between the pressure and the velocity, a suitable anemometer of either class will give information about both these quantities. The velocity of an object is simply its speed in a particular direction. ... The use of water pressure - the Captain Cook Memorial Jet in Lake Burley Griffin, Canberra. ...

The first anemometer was invented by Leone Battista Alberti in the 15^th century. Statue of Leon Battista Alberti. ...

Anemometer installation on roof of Deconism Gallery, using three size 6, schedule 40 pipes in their original uncut 20 foot (6 m) lengths. The wire (4 conductors running inside a shield) runs along the rightmost leg of the 3 legged "tripod" mount that's attached to the rigging that runs around the perimeter of the roof.

Download high resolution version (1524x2376, 97 KB)Anemometer atop the roof of Deconism Gallery I took this picture Saturday September 18th, just before sunset, from the roof of Deconism Gallery, using Nikon D2h, 18-70mm zoom lens, set to widest (18mm), and over exposed approximately 2 f stops from meter... Download high resolution version (1524x2376, 97 KB)Anemometer atop the roof of Deconism Gallery I took this picture Saturday September 18th, just before sunset, from the roof of Deconism Gallery, using Nikon D2h, 18-70mm zoom lens, set to widest (18mm), and over exposed approximately 2 f stops from meter...

Velocity anemometers

Cup anemometers

The simplest type of anemometer is the cup-anemometer, invented by Robert Hooke. One particular good thing about the cup anemometer is its simplicity. But if you use it without electronic data logging equipment it isn't very good at leaving a record of the actual speed at any particular moment, and so it can leave very brief events unrecorded. Unfortunately, when Dr. Robert first designed his anemometer, he stated that no matter what the size of the cups or the length of the arms, the cups always moved with one-third of the speed of the wind. This result was apparently confirmed by some early independent experiments, but it is very far from the truth. It was later discovered that the actual relationship between the speed of the wind and that of the cups depends very largely on the dimensions of the cups and arms, and may have almost any value between two and a little over three. This had the result that wind speeds published in many official 19th century publications were often in error by nearly 60%.

Hot-wire anemometers

Hot-wire anemometers use a very fine wire (on the order of several micrometers) heated up to some temperature above the ambient. Flow past the wire has a cooling effect on the wire. As the electrical resistance of most metals (tungsten is a popular choice for hot-wires) is dependent upon the temperature of the metal, a relationship can be obtained between the resistance of the wire and the flow velocity.^[1]

Several ways of implementing this exist, and hotwires can be further classified as CCA (Constant-Current Anemometer), CVA (Constant-Voltage Anemometer) and CTA (Constant-Temperature Anemometer). The voltage output from these anemometers is thus the result of some sort of circuit within the device trying to maintain the specific variable (Current, Voltage or Temperature) constant.

Additionally, PWM (Pulse-Width Modulated) anemometers are also used, wherein the velocity is inferred by the time length of a repeating pulse of current that brings the wire up to a specified resistance and then stops until a threshold "floor" is reached, at which time the pulse is sent again.

Hot-wire anemometers, while extremely delicate, have extremely high frequency-response and fine spatial resolution compared to other measurement methods, and as such are almost universally employed for the detailed study of turbulent flows, or any flow in which rapid velocity fluctuations are of interest.

Laser Doppler anemometers

Laser Doppler anemometers use a laser beam that is split and sent out of the anemometer. The backscatter of the laser beam off of air molecules is directed into a detector where the relative velocity between the laser in the anemomter and the backscattered radiation is compared to determine the volocity of the air molecules.^[2]

Drawing of a laser anemomter. The laser is emitted (1) through the front lense (6) of the anemomerter and is backscattered off the air molecules (7). The backscattered radiation (dots) re-enter the device and are reflected and directed into a detector (12).

Image File history File links Download high-resolution version (1186x588, 207 KB) File links The following pages on the English Wikipedia link to this file (pages on other projects are not listed): Anemometer ... Image File history File links Download high-resolution version (1186x588, 207 KB) File links The following pages on the English Wikipedia link to this file (pages on other projects are not listed): Anemometer ...

Sonic anemometers

Sonic anemometers use sound waves (ultrasonic) to measure wind speed and direction. They are capable of measuring wind velocity in the X (east-west), Y (north-south), and Z (up-down) directions. The spatial resolution is given by the path length between transducers, which is typically 10 to 20 cm. Sonic anemometers can take measurements with very fine temporal resolution, 20 Hz or better, which make them well suited for turbulence measurements. The lack of moving parts makes them appealing to automated weather stations. Their main disadvantage lie in the distortion of the flow itself by the structure supporting the six transducers. This distortion has to be determined by a comprehensive 3D investigation in a wind tunnel in order to obtain accurate wind measurements. Use of such anemometers is likely to increase in the future, both for meteorological stations and for e.g. for wind turbine control systems. // CM, cM, Cm or cm may stand for: CM Apollo Command/Service Module (command module is one half) Cameroon, ISO and FIPS country code category management Catholic Memorial center of mass Championship Manager, a series of association football computer games Chelmsford British post code region CM Chessmaster Chief Minister of... Hz or hz may mean: Herero language (ISO 639 alpha-2, hz) Hertz, unit of frequency This is a disambiguation page — a list of articles associated with the same title. ... In fluid dynamics, turbulence or turbulent flow is a flow regime characterized by chaotic, stochastic property changes. ...

Windmill anemometers

Anemometer with vertical axis and turnabout counter. Dubendorf musseum of military aviation

An aerovane

The other forms of mechanical velocity anemometer may be described as belonging to the windmill type. In the Robinson anemometer the axis of rotation is vertical, but with this subdivision the axis of rotation must be parallel to the direction of the wind and therefore horizontal. Furthermore, since the wind varies in direction and the axis has to follow its changes, a wind vane or some other contrivance to fulfill the same purpose must be employed. An aerovane combines a propeller and a tail on the same axis to obtain accurate and precise wind speed and direction measurements from the same instrument. In cases where the direction of the air motion is always the same, as in the ventilating shafts of mines and buildings for instance, wind vanes, known as air meters are employed, and give most satisfactory results. Image File history File linksMetadata Anemometer_dubendorf. ... Image File history File linksMetadata Anemometer_dubendorf. ... Dübendorf is a suburb of Zürich in Switzerland with a population of about 22,700 (2004). ... Image File history File links Download high resolution version (1824x1208, 989 KB) Description: Project Vortex mesonet vehicle aerovane for wind speed and direction. ... Image File history File links Download high resolution version (1824x1208, 989 KB) Description: Project Vortex mesonet vehicle aerovane for wind speed and direction. ... Spanish Windmills at La Mancha A windmill is an engine powered by the wind to produce energy, often contained in a large building as in traditional post mills, smock mills and tower mills. ... Weather vane Weather cock Aerovane A weather vane, also called a wind vane, is a movable device attached to an elevated object such as a roof for showing the direction of the wind. ...

Pressure anemometers

The first designs of anemometers which measure the pressure were divided into plate and tube classes.

Plate anemometers

The simplest type of this form consists of a flat plate, which is usually square or circular, while a wind vane keeps this exposed normally to the wind, and the pressure of the wind on its face is balanced by a spring. The distortion of the spring determines the actual force which the wind is exerting on the plate, and this is either read off on a suitable gauge, or leaves a record via a data logger. Instruments of this kind are inaccurate for high wind readings, and are poor at recording variable winds.

Tube anemometers

Anemometers

Lind's anemometer, which consists simply of a U tube containing liquid with one end bent into a horizontal direction to face the wind, is perhaps the original form from which the tube class of instrument has sprung. If the wind blows into the mouth of a tube it causes an increase of pressure inside and also of course an equal increase in all closed vessels with which the mouth is in airtight communication. If it blows horizontally over the open end of a vertical tube it causes a decrease of pressure, but this fact is not of any practical use in anemometry, because the magnitude of the decrease depends on the wind striking the tube exactly at right angles to its axis, the most trifling departure from the true direction causing great variations in the magnitude. The pressure tube anemometer (fig. 1) utilizes the increased pressure in the open mouth of a straight tube facing the wind, and the decrease of pressure caused inside when the wind blows over a ring of small holes drilled through the metal of a vertical tube which is closed at the upper end. The pressure differences on which the action depends are very small, and special means are required to register them, but in the ordinary form of recording anemometer (fig. 2), any wind capable of turning the vane which keeps the mouth of the tube facing the wind is capable of registration. Image File history File links Anemometers. ... Image File history File links Anemometers. ...

The great advantage of the tube anemometer lies in the fact that the exposed part can be mounted on a high pole, and requires no oiling or attention for years; and the registering part can be placed in any convenient position, no matter how far from the external part. Two connecting tubes are required. It might appear at first sight as though one connection would serve, but the differences in pressure on which these instruments depend are so minute, that the pressure of the air in the room where the recording part is placed has to be considered. Thus if the instrument depends on the pressure or suction effect alone, and this pressure or suction is measured against the air pressure in an ordinary room, in which the doors and windows are carefully closed and a newspaper is then burnt up the chimney, an effect may be produced equal to a wind of 10 mi/h (16 km/h); and the opening of a window in rough weather, or the opening of a door, may entirely alter the registration.

Notes on wind measurements

In the tube anemometer also it is really the pressure that is measured, although the scale is usually graduated as a velocity scale. In cases where the density of the air is not of average value, as on a high mountain, or with an exceptionally low barometer for example, an allowance must be made. Approximately 1½% should be added to the velocity recorded by a tube anemometer for each 1000 ft (5% for each kilometer) that it stands above sea-level.

Anemometers, such as the one shown above at Deconism Gallery, are often used in conjunction with windmills, so that the wind speed and power generated by the turbine (windmill) can be logged together in a data logger.

Other types of anemometers include:

• hot wire or hot plate sensors, which measure the cooling of a heated element immersed in the wind
• ultrasonic sensors, which measure the Doppler shift of sound waves travelling across the moving air
• laser anemometers, which measure the velocity of particles passing through fringes formed by the intersection of two laser beams

The Doppler effect is the apparent change in frequency or wavelength of a wave that is perceived by an observer moving relative to the source of the waves. ...

See also

• Anemoscope, ancient device for measuring or predicting wind direction or weather
• Windsock, device for measuring wind speed and direction
• Weather vane, device for indicating wind direction

An anemoscope is an obsolete machine invented to show the direction of the wind, or to foretell a change of wind direction or weather. ... A windsock is a large, conical, open-ended tube designed to indicate wind direction and relative wind speed. ... Weather vane Weather cock Aerovane A weather vane, also called a wind vane, is a movable device attached to an elevated object such as a roof for showing the direction of the wind. ...

References

Supporters contend that the Eleventh Edition of the Encyclopædia Britannica (1910-1911) represents the sum of human knowledge at the beginning of the 20th century; indeed, it was advertised as such. ... September 18 is the 261st day of the year (262nd in leap years). ... 2006 (MMVI) is a common year starting on Sunday of the Gregorian calendar. ... June 29 is the 180th day of the year (181st in leap years) in the Gregorian Calendar, with 185 days remaining. ... 1976 (MCMLXXVI) was a leap year starting on Thursday. ... September 18 is the 261st day of the year (262nd in leap years). ... 2006 (MMVI) is a common year starting on Sunday of the Gregorian calendar. ...

External links

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Anemometer

• Glossary Definition: Anemometer - AMS Glossary of Meteorology
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