Windcatcher

An ab anbar (water reservoir) with double domes and windcatchers (openings near the top of the towers) in the central desert city of Yazd, Iran

A windcatcher (wind tower, wind scoop) is a traditional architectural element used to create natural ventilation and passive cooling in buildings.[1] Windcatchers come in various designs: unidirectional, bidirectional, and multidirectional. Windcatchers are widely used in North Africa and in the West Asian countries around the Persian Gulf, and have been for the past three thousand years.[2] Neglected by modern architects in the latter half of the 20th century, the early 20th century saw them used again, to increase ventilation and cut power demand and costs for air-conditioning.

Structure and functionEdit

This wind tower has four openings and brown cloth vertical walls on the interior diagonals, so it can catch the wind from a range of directions (inside view). Dubai Museum.
More frequently, wind towers are masonry, like this eight-sectioned example in Souq Waqif, Doha, Qatar
Malqafs in Egypt in 1878; short right triangular prisms with the vertical side left open and facing directly up or down wind (one of each per building). This works in areas with strong low-level winds from a consistent direction.

Windcatchers vary dramatically in shape, including height, cross-sectional area, and internal sub-divisions and filters.[2]

The construction of a windcatcher depends on the prevailing wind direction at that specific location: if the wind tends to blow from only one side, it may have only one opening, and no internal partitions.[2] In areas with more variable wind directions, there may also be radial internal walls, which divide the windtower into vertical sections. These sections are like parallel chimneys, but with openings to the side, pointing in multiple directions.[2] More sections reduce the flow rate, but increase the efficiency at suboptimal wind angles. If the wind hits the opening square, on, it will go in, but if it hits it at a sufficiently oblique angle, it will tend to slip around the tower, instead.[2]

Windcatchers in areas with stronger winds will have smaller total cross-sections,[3] and areas with very hot wind may have many smaller shafts in order to cool the incoming air.[4]:Ch. 5 Windtowers with square horizontal cross-sections are more efficient than round ones, as the sharp angles make the flow less laminar, encouraging flow separation;[2] suitable shaping increases suction.[4]:Ch. 5

Taller windcatchers catch higher winds. Higher winds blow stronger and cooler[5] (and in a different direction).[citation needed] Higher airs are also usually less dusty.[5]

If the wind is dusty or polluted, or there are insect-borne illnesses such as malaria and dengue fever, then air filtering may be necessary.[2] Some dust can be dumped at the bottom of the windcatcher as the air slows (see diagram), and more can be filtered out by suitable plantings or insect mesh.[5] Physical filters generally reduce throughflow, unless the flow is very gusty.[2] It may also be possible to fully or partially close the windcatcher off.[3]

The short, wide right-triangle-prism malqaf are usually bidirectional, set in symmetrical pairs, and are often used with a salasaibil (evaporative cooling unit)[2] and a shuksheika (roof lantern vent).[5] Wide malqafs are more often used in damper climates, where high-volume air flow is more important compared to evaporative cooling. In hotter climates, they are narrower, and air is cooled on its way in.[4]:Ch. 5 They are more commonly used in Africa.[2] Baudgir, on the other hand, are multisided (usually 4-sided), and they are typically tall towers (up to 34 meters tall) which can be closed in winter. They are more common in the Gulf region[2] and in areas with dust storms.[3] Taller windcatchers also have a stronger stack effect.[4]:Ch. 5

Windcatching has gained some ground in Western architecture, and there are several commercial products using the name windcatcher. Some modern windcatchers use sensor-controlled moving parts or even solar-powered fans to make a semi-passive ventilation system.[2]

Windscoops have long been used on ships.[6][better source needed] Windcatchers have also been used experimentally to cool outdoor areas in cities, with mixed results;[2] traditional methods include narrow, walled spaces, parks and winding streets, which act as cold-air reservoirs (see section on night flushing, below).[4]:Ch. 6

Cooling methodsEdit

Night-flushing cools the house by increasing ventilation at night, when the outdoor air is cooler;[5] windtowers can assist night flushing.[citation needed]

A windcatcher can also cool air by drawing it over cool objects. In arid climates, the daily temperature swings are often extreme, with desert temperatures often dipping below freezing night. The thermal inertia of the soil evens out the daily and even annual temperature swings. Even the thermal inertia of thick masonry walls will keep a building warmer at night and cooler during the day. Windcatchers can thus cool by drawing air over night- or winter-cooled materials, which act as heat reservoirs.

Windcatchers that cool by drawing air over water use the water as a heat reservoir, but if the air is dry, they are also cooling the air with evaporative cooling.[2] The heat in the air goes into evaporating some of the water, and will not be released until the water re-condenses. This is a very effective way of cooling dry air.[2]

Simply moving the air also has a cooling effect. Humans cool themselves using evaporative cooling when they sweat. A draft disrupts the boundary layer of body-warmed and water-saturated air clinging to the skin, so a human will feel cooler in moving air than in stagnant air of the same temperature.[4]:Ch. 5

Forces to move airEdit

 
A pair of short windcatchers or malqaf used in traditional architecture; wind is forced down on the windward side and leaves on the leeward side. In the center, a shuksheika (roof lantern vent), used to shade the courtyard below while allowing hot air rise out of it.[5]

The windcatcher can function in two ways: directing airflow using the pressure of wind blowing into the windcatcher, or directing airflow using buoyancy forces from temperature gradients (stack effect). The relative importance of these two forces has been debated. The importance of windpressure obviously increases with increasing wind speed, and is generally more important than buoyancy under most conditions in which the windcatcher is working effectively.[2]

Airflow from wind pressureEdit

One of the most common uses of the windcatcher is to cool the inside of the dwelling; it is often used in combination with courtyards and domes as an overall ventilation and heat-management strategy. The windcatcher's open side faces the prevailing wind, thus "catching" it, and brings it down into the heart of the building, maintaining a draft, and thus cooling the people in the building interior. It does not necessarily cool the air itself; the rate of airflow itself can provide a cooling effect. The air swirls through the house, and leaves from the other side, creating a through-draft.[citation needed] The suction Windcatchers have been employed in this manner for thousands of years.[4]

Suction from the lee side of a windtower is also an important driving force, usually somewhat more constant and less gusty than the pressure on the upwind side.(see Venturi effect and Bernoulli's principle).[4]:Ch. 5

Windtowers topped with horizontal airfoils have been built to enhance these pressure gradients.[2] The shape of the shuksheika roof also creates suction as wind blows over it.[4]:Ch. 5

Airflow from convectionEdit

 
Vertical temperature gradient cause by stable stratification of air inside a room. Note hot air rising from the person.

Buoyancy is usually not the main effect driving windcatcher air circulation[2] during the day.

In a windless environment, a windcatcher can still function using the stack effect[5]. The hot air, which is less dense, tends to travel upwards and escape out the top of the house via the windtower. Heating of the windtower itself can heat the air inside (making it a solar chimney), so that it rises and pulls air out of the top of the house, creating a draft. This effect can be enhanced with a heat source at the bottom of the windtower (such as humans, ~80 Watts each[citation needed]}, but this heats the house and makes it less comfortable.[2]

A takhtabush is a space similar to the ancient Roman tablinum, with openings from both a heavily-shaded courtyard and a slightly less-shaded rear garden. It has a strong cross-breeze from the courtyard, at least partly driven by convection;[4]:Ch. 6[5] it thus uses the courtyard somewhat like a wind tower.

Buoyancy forces are used to cause night flushing (see below).

Night flushingEdit

The diurnal temperature cycle means that the night air is colder than the daytime air; in arid climates, much colder. This creates appreciable buoyancy forces. Buildings may be designed to spontaneously increase ventilation at night.

Courtyards in hot climates fill with cold air at night. This cold air then flows from the courtyard into adjacent rooms.[5] The cold night air will flow in easily, as it is more dense than the rising warm air it is displacing.[4]:Ch. 6[5] But in the day, the courtyard walls and awning shade it, while the air outside is heated by the sun.[5] The cool masonry will also chill the nearby air.[7] The courtyard air will become stably stratified,[citation needed] the hot air floating on top of the cold air with little mixing.[4]:Ch. 6 The fact that the openings are at the top will trap the cool air below, though it cannot cause the temperature to drop below the nightly minimum temperature. This mechanism also works in windtowers.[3]

Subterranean coolingEdit

 
A shabestan, a cool earth-sheltered room which may be ventilated with windcatchers. The fountain pool adds evaporative cooling.

A windcatcher can also cool air by bringing into contact with cool thermal masses. These are often found underground.

Below approximately 6m of depth, soil and groundwater is always at about the annual mean-average temperature (MATT)[8][9][10] (it is this depth which is used for many ground-source heat pumps, often loosely referred to as "geothermal heat pumps" by laypeople[11]). Below approximately 6m of depth, soil and groundwater is always at about the annual mean-average temperature (MATT)[12][13][14] (it is this depth which is used for many ground-source heat pumps, often loosely referred to as "geothermal heat pumps" by laypeople[11]). The thermal inertia of the soil evens out the daily and even annual temperature swings. In arid climates, the daily temperature swings are often extreme, with desert temperatures often dipping below freezing at night. Even the thermal inertia of thick masonry walls will keep a building warmer at night and cooler during the day; in hot-arid climates, thick walls with high thermal mass (adobe, stone, brick) are common (though thinner walls with high resistance against heat transmission are more modernly sometimes used).[5] Windcatchers can thus cool by drawing air over night- or winter-cooled materials, which act as heat reservoirs.

Windcatchers are also often used to ventilate lower-level indoor spaces (e.g. shabestans), which maintain frigid temperatures in the middle of the day even without windcatchers. Ice houses are traditionally used to store water frozen overnight in desert areas, or over winter in temperate areas. They may use windcatchers to circulate air into an underground or semi-underground chamber, evaporatively cooling the ice so that it melts only slowly and stays fairly dry (see lede image). At night, the windcatchers may even bring sub-freezing night air underground, helping to freeze ice.

Evaporative coolingEdit

 
A windcatcher and qanat used for cooling

In dry climates, the evaporative cooling effect may be used by placing water at the air intake, such that the draft draws air over water and then into the house. For this reason, it is sometimes said that the fountain, in the architecture of hot, arid climates, is like the fireplace in the architecture of cold climates.[5]

Windcatchers are used for evaporative cooling in combination with a qanat, or underground canal (thich also makes use of the subterranean heat reservoir described above). In this method, the open side of the tower faces away from the direction of the prevailing wind (the tower's orientation may be adjusted by directional ports at the top). When only the leeward side is left open, air is drawn upwards using the Coandă effect. This sucks air into an intake on the other side of the building. The hot air is brought down into the qanat tunnel and is cooled by coming into contact with the cool earth[Note 1] and the cold water running through the qanat. The air is also evaporatively cooled when some of the water in the qanat evaporates as the hot, dry surface air passes over it; the heat energy in the air is absorbed as energy of vaporization. The dry air is thus also humidified before entering the building. The cooled air is drawn up through the house and finally out the windcatcher, again by the Coandă effect. On the whole, the cool air flows through the building, decreasing the structure's overall temperature.

A salasabil is a vertical wall plate with a thin sheet of water flowing over it, and thence usually via a channel to a basin. A salasabil or other fountain can also be used to evaporatively cool air.[5][4]:Ch. 7

Wetted matting can also be hung inside the windcatcher to cool incoming air.[5] This can reduce flow, especially in weak winds. However, it can also produce a downdraft of cool air in windless conditions.[2]

Regional useEdit

AfricaEdit

In Egypt windcatchers are known as malqaf, pl. malaaqef.[15][16][17] They are generally shaped as right triangular prisms with the vertical side left open and facing directly up or down wind (one of each per building). They work best if oriented within 10 degrees of wind direction; larger angles allow the wind to escape.[17] Windcatchers were used in traditional ancient Egyptian architecture,[18] and only started to fall out of use in the mid-1900s C.E.. Their use is now being re-examined, as air conditioning accounts for 60% of Egypt's peak electrical power demand (and thus the need for 60% of its generating capacity).[17]

Windcatchers in Egypt are often used in conjunction with other passive cooling elements.[5]

Middle East and AsiaEdit

IranEdit

In Iran, a windcatcher is called a bâdgir: bâd "wind" + gir "catcher" (Persian: بادگیر‎). The devices were used in Achaemenid architecture.[3] In Iran, they are used in the hot, dry areas of the Central Plateau, and in the hot, humid coastal regions.[3]

Central Iran shows large diurnal temperature variation with an arid climate. Most buildings are constructed from thick ceramic with high insulation values. Towns centered on desert oases tend to be packed very closely together with high walls and ceilings, maximizing shade at ground level. The heat of direct sunlight is minimized with small windows that face away from the sun.[3]

The windcatcher's effectiveness had led to its routine use as a refrigerating device in Iran. Many traditional water reservoirs (ab anbars), which are capable of storing water at near freezing temperatures during summer months, are built with windcatchers.[3] The evaporative cooling effect is strongest in the driest climates, such as on the Iranian plateau, leading to the ubiquitous use of windcatchers in drier areas such as Yazd, Kerman, Kashan, Sirjan, Nain, and Bam.

Windcatchers tend to have one, four, or eight openings. In the city of Yazd, all windcatchers are four- or eight-sided. The construction of a windcatcher depends on the direction of airflow at that specific location: if the wind tends to blow from only one side, it is built with only one downwind opening. This is the style most commonly seen in Meybod, 50 kilometers from Yazd: the windcatchers are short and have a single opening.

Windcatchers in Iran may be quite elaborate, due to their use as status symbols.[3]

A small windcatcher is called a shish-khan in traditional Persian architecture. Shish-khans can still be seen on top of ab anbars in Qazvin and other northern cities in Iran. These seem to function more as ventilators than as the temperature regulators seen in the central deserts of Iran.

QatarEdit

 
The University of Qatar in Doha has unusual windcatchers.[2]

PakistanEdit

 
Simple windcatchers in Hydrabad in the 1800s

AustraliaEdit

 
Council House 2. Wind towers in concrete canyon to the left.

Council House 2 in Melbourne, Australia, has 3-story-tall "shower towers", made of cloth kept wet by a showerhead trickling at the top of each one. Evaporative cooling chills the air, which then descends into the building.[7]

EuropeEdit

 
The Zénith de Saint-Étienne Métropole has an extremely wide aluminium windcatcher scoop.

The Saint-Étienne Métropole's Zénith is a multi-purpose hall built in Auvergne-Rhône-Alpes (inland southern France). It incorporates a very large aluminium windcatcher,[19] which is much lighter than the equivalent masonry windcatcher would be. The size of the windcatcher allows it to work in any wind direction;[19] the cross-sectional area perpendicular to the wind flow remains large.

The Bluewater Shopping Centre in the UK uses windcatcher towers.[7] The Queen’s Building of DeMontfort University uses stack-effect towers to ventilate.[20]

AmericasEdit

 
The Kensington Oval cricket ground in Barbados also uses a very wide aluminium windscoop.[19]

A windcatcher has been used in the visitor center at Zion National Park, Utah,[21] where it functions without the addition of mechanical devices in order to regulate temperature.[19]

See alsoEdit

NotesEdit

  1. ^ The earth stays cool by virtue of being several meters below the surface. The insulation and heat capacity of the overlying earth maintains the same stable temperature day and night, and as nights in arid climate are quite cold, often below freezing, that stable temperature is quite cool.

ReferencesEdit

  1. ^ Malone, Alanna. "The Windcatcher House". Architectural Record: Building for Social Change. McGraw-Hill.
  2. ^ a b c d e f g h i j k l m n o p q r s t u Saadatian, Omidreza; Haw, Lim Chin; Sopian, K.; Sulaiman, M.Y. (April 2012). "Review of windcatcher technologies" (PDF). Renewable and Sustainable Energy Reviews. 16 (3): 1477–1495. doi:10.1016/j.rser.2011.11.037.
  3. ^ a b c d e f g h i A. A'zami (May 2005). "Badgir in traditional Iranian architecture" (PDF). International Conference "Passive and Low Energy Cooling 1021 for the Built Environment", May 2005, Santorini, Greece. Retrieved 21 March 2012. (the English is hard to understancd)
  4. ^ a b c d e f g h i j k l m Fathy, Hassan. "The wind factor in air movement". Natural Energy and Vernacular Architecture.
  5. ^ a b c d e f g h i j k l m n o p Mohamed, Mady A. A. (2010). S. Lehmann, H.A. Waer, and J. Al-Qawasmi (eds.). Traditional Ways of Dealing with Climate in Egypt (PDF). The Seventh International Conference of Sustainable Architecture and Urban Development (SAUD 2010). Sustainable Architecture and Urban Development. Amman, Jordan: The Center for the Study of Architecture in Arab Region (CSAAR Press). pp. 247–266.CS1 maint: uses editors parameter (link) (bw version)
  6. ^ Richter, Jim (2003). "Liberty Ship Photo".
  7. ^ a b c "Whither the Windcatcher?". Conservation. 23 May 2012.
  8. ^ "Groundwater temperature's measurement and significance - National Groundwater Association". National Groundwater Association. 23 August 2015.
  9. ^ "Mean Annual Air Temperature - MATT". www.icax.co.uk.
  10. ^ "Ground Temperatures as a Function of Location, Season, and Depth". builditsolar.com.
  11. ^ a b Rafferty, Kevin (April 1997). "An Information Survival Kit for the Prospective Residential Geothermal Heat Pump Owner" (PDF). Geo-Heat Centre Quarterly Bulletin. 18 (2). Klmath Falls, Oregon: Oregon Institute of Technology. pp. 1–11. ISSN 0276-1084. Archived from the original (PDF) on 17 February 2012. Retrieved 2009-03-21. The author issued an updated version of this article in February 2001.
  12. ^ "Groundwater temperature's measurement and significance - National Groundwater Association". National Groundwater Association. 23 August 2015.
  13. ^ "Mean Annual Air Temperature - MATT". www.icax.co.uk.
  14. ^ "Ground Temperatures as a Function of Location, Season, and Depth". builditsolar.com.
  15. ^ Ahmed Abdel Wahab Ahmed Rizk; Mohamed Abdel Mawgoud Abdel Ghaffar; Mohamed Hefnawy (11 April 2007). "The effect of wind-catchers (el-Malaqef) on the internal natural ventilation in hot climates with special reference to Egypt: A study on small physical models" (Microsoft Word document (.doc)). www.aun.edu.eg (in English and Arabic). Asyut: Assiut University. p. 1. Retrieved 21 September 2016. EL-MALAQEF
  16. ^ "Industrial architecture in Egypt in the 19th and 20th centuries, Arsenal in the Citadel of Cairo: workshop hall with timber roof construction and wind catcher (malqaf)". Dainst.org. Archived from the original on 2013-05-13. Retrieved 2013-04-22.
  17. ^ a b c Shady Attia (2–24 June 2009). Designing the Malqaf for summer cooling in low-rise housing, an experimental study (PDF). 26th Conference on Passive and Low Energy Architecture (PLEA2009). Retrieved 2013-04-22.CS1 maint: date and year (link) CS1 maint: date format (link)
  18. ^ Air-conditioning avoidance Archived October 23, 2007, at the Wayback Machine
  19. ^ a b c d "How Ancient Persian Architecture Captured Wind Energy Underground to Green Buildings". This Big City.net. Retrieved 21 March 2012.
  20. ^ "Queen's Building, DeMontfort University" (PDF).
  21. ^ "Zion Canyon Visitor Center". National Park Service - Zion National Park. Retrieved 2018-10-29.

External linksEdit