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A dust storm or sandstorm is a meteorological phenomenon common in arid and semi-arid regions. Dust storms arise when a gust front blows loose sand and dust from a dry surface. Particles are transported by saltation and suspension, causing soil erosion from one place and deposition in another. The Sahara and drylands around the Arabian peninsula are the main source of airborne dust, with some contributions from Iranmarker, Pakistanmarker and Indiamarker into the Arabian Seamarker, and China'smarker storms deposit dust in the Pacificmarker. It has been argued that recently, poor management of the Earth's drylands, such as neglecting the fallow system, are increasing dust storms from desert margins and changing both the local and global climate, and also impacting local economies.

The term sandstorm is used most often in the context of desert sandstorms, especially in the Sahara, when, in addition to fine particles obscuring visibility, a considerable amount of larger sand particles are blown closer to the surface. The term dust storm is more likely to be used when finer particles are blown long distances, especially when the dust storm affects urban areas.

Causes

As the force of wind passing over loosely held particles increases, particles of sand first start to vibrate, then to saltate ("leap"). As they repeatedly strike the ground, they loosen smaller particles of dust which then begin to travel in suspension. At wind speeds above that which causes the smallest to suspend, there will be a population of dust grains moving by a range of mechanisms: suspension, saltation and creep.

A recent study finds that the initial saltation of sand particles induces a static electric field by friction. Saltating sand acquires a negative charge relative to the ground which in turn loosens more sand particles which then begin saltating. This process has been found to double the number of particles predicted by previous theory.
Particles become loosely held mainly due to drought or arid conditions, and wind has varied causes. Gust fronts may be produced by the outflow of rain-cooled air from an intense thunderstorm, or they may represent a dry cold front, that is, a cold front that is moving into a dry air mass and is producing no precipitation. This is the type of dust storm which was common during the Dustbowl years in the U.S. Following the passage of a dry cold front, convective instability resulting from cooler air riding over heated ground can maintain the dust storm initiated at the front. In desert areas, dust and sand storms are most commonly caused by either thunderstorm outflows, or by strong pressure gradients which cause an increase in wind velocity over a wide area. The vertical extent of the dust or sand that is raised is largely determined by the stability of the atmosphere above the ground as well as by the weight of the particulates. In some cases, dust and sand may be confined to a relatively shallow layer by a low-lying temperature inversion. In other instances, dust (but not sand) may be lifted as high as 20,000 feet (6,100 m) high.

Drought and wind contribute to the emergence of dust storms, as do poor farming and grazing practices by exposing the dust and sand to the wind.

Dryland farming is also another cause of dust storms, since dryland farmers rely on rainfall to water their crops, they engage in practices to maintain moisture in the soil. Such practices include leaving a field fallow for a year after harvesting to allow the buildup of water to build in the soil and covering the field with dry earth in an attempt to seal in the underlying. These practices make dryland agriculture susceptible to dust storms. These methods are used by farmers in eastern Washingtonmarker, an arid region.

Physical and environmental impacts

Animation showing the global movement of dust from an Asian dust storm.
Dust from the Sahara moves into the North Atlantic.


A sandstorm can move whole sand dunes. Dust storms can carry large amounts of dust, so much so that the leading edge of one can appear as a solid wall of dust as much as 1.6 km (1 mile) high. Dust and sand storms which come off the Sahara Desert are locally known as a simoom or simoon (sîmūm, sîmūn). The haboob (həbūb) is a sandstorm prevalent in the region of Sudanmarker around Khartoummarker. When it happens you cant see even a thing but a wall of sand covering your view.

The Sahara desert is a key source of dust storms, particularly the Bodélé Depression and an area covering the confluence of Mauritaniamarker, Malimarker, and Algeriamarker.

Saharan dust storms have increased approximately 10-fold during the half-century since the 1950s, causing topsoil loss in Nigermarker, Chadmarker, northern Nigeriamarker, and Burkino Fasomarker. In Mauritania there were just two dust storms a year in the early 1960s, but there are about 80 a year today, according to Andrew Goudie, a professor of geography at Oxford University. Levels of Saharan dust coming off the east coast of Africa in June (2007) were five times those observed in June 2006, and were the highest observed since at least 1999, which may cool Atlantic waters enough to slightly reduce hurricane activity in late 2007.

Dust storms have also been shown to increase the spread of disease across the globe. Virus spores in the ground are blown into the atmosphere by the storms with the minute particles then acting like urban smog or acid rain.

Economic impact

Dust storms cause soil loss from the dry lands, and worse, they preferentially remove organic matter and the nutrient-rich lightest particles, thereby reducing agricultural productivity. Also the abrasive effect of the storm damages young crop plants. Other effects that may impact the economy are: reduced visibility affecting aircraft and road transportation; reduced sunlight reaching the surface; increased cloud formation increasing the heat blanket effect; high level dust sometimes obscures the sun over Florida; effects on human health of breathing dust.

Dust can also have beneficial effects where it deposits: Central and South American rain forests get most of their mineral nutrients from the Sahara; iron-poor ocean regions get iron; and dust in Hawaii increases plantain growth. In northern China as well as the mid-western U.S., ancient dust storm deposits known as loess are highly fertile soils, but they are also a significant source of contemporary dust storms when soil-securing vegetation is disturbed.

Extraterrestrial dust storms

See Mars Dust Storms.

Notable dust storms



  • ~524BC The 50,000 strong army of Cambyses II supposedly buried by a sandstorm en route to the Siwa Oasismarker.
  • 1930s: A series of dust storms displaced hundreds of thousands of agricultural workers in the central United Statesmarker and Canadamarker during the Dust Bowl.
  • 1934: Just one of many notable storms in the 1930s, the storm of 9-11 May 1934 began in the far north-western Great Plains and proceeded east over the northern tier of states and parts of Canada and was notable for removing the vast majority of the soil deposited since the last Ice Age over some parts of its path.
  • 1935: Another major dust bowl storm took place on April 14, which became known as Black Sunday.
  • 1954-1991: The multi-year droughts in portions of North America of 1954-56, 1976-78, and 1987-91 were noted for dust storms of the intensity seen in the middle 1930s over some fraction of their coverage and timespan, and more sporadically during the times between. The three multi-year droughts were similar to the 1930s in storms being raised by synoptic scale weather events such as cyclones and cold fronts; otherwise the most common trigger is the outflow from convective activity, known as a haboob. Significant events of the latter variety occurred in Colorado and Kansas in May 2004 with winds to 100 mph, Minnesota and Wisconsin in June 2004 causing significant damage, and the upper Middle West in May 1988, notable for strong electrification and lightning activity and by one estimate reaching 30 000 ft or more. The first and third of this list reached black blizzard intensity, causing total blackout for some period ranging from 90 sec to 10 or more minutes, over some fraction of the ground covered. The 1987-91 drought was especially notable as in the 1930s for the large number of rain of mud events, often generated by dust in suspension and/or carried on upper-level winds.
  • 1971: A dust storm that occurred near Tucson, Arizona on July 16 was extensively documented by meteorologists.
  • 1983: 1983 Melbourne dust storm: On the afternoon of February 8 a huge dust storm originating in the Mallee region of Victoriamarker, Australia covered the city of Melbournemarker.
  • 2007: On Saturday afternoon February 24, a large dust storm originating in the West Texasmarker area of Amarillomarker covered much of the North Texas area. Strong winds caused extensive property damage to fences, roof shingles, and some buildings. The DFW Airportmarker was severely affected, causing extensive flight delays into and out of the DFW area. Area residents suffered respiratory problems and allergic reactions, causing many people to visit hospitals. This event was also marked by relative humidities down to 1 per cent, in one case the juxtaposition of a c. 70°F air temp and dew point of -20°F, in and around of the area affected.
  • 2007: In June, a large dust storm generated by Cyclone Yemyin struck Karachi Pakistan and areas of the Sindh and lower Balochistan, followed by a series of heavy rainfalls which resulted in a death toll of nearly 200.
  • 2008: On February 11, a sandstorm in the Kingdom of Bahrainmarker in Sakhir halted Formula One testing for Ferrarimarker, BMW Sauber and Toyota
  • 2009: 2009 Australian dust storm: On September 23, a dust storm that started in South Australiamarker and inland New South Walesmarker, Australia, blanketed New South Walesmarker with reddish orange skies. It stretched as far north as southern Queenslandmarker.


Gallery

Image:Sahara dust plume Nov 1998.jpg|Dust plume off the Sahara desert over the northeast Atlantic Ocean.Image:Cyprus.A2002292.1045.500m.jpg|Dust storm moving over Cyprusmarker from the rest of the Middle East.Image:Dust storm in Wagga Wagga.jpg|Dust storm in Wagga Wagga, New South Walesmarker, Australia.Image:Sydney harbour bridge duststorm.jpg|Dust storm in Sydneymarker, Australia.Image:Zandstorm.jpg|Dust storm in Burkina Fasomarker.Image:Sandsturm-2.jpg|Storm in Erfoudmarker, Moroccomarker.File:Sandstorm Fallujah 2006.JPG|A massive sandstorm rolling through Fallujah, Iraq in 2006Image:Dust Storm over Iraq.jpg|Dust storm over Iraq, July 30, 2009.File:Iraq_dust_storm_20090705.ogg|Enormous dust storm emerging in Iraq and crossing Iran.Image:GCDustStorm.JPG|Dust Storm in Surfers Paradise, Australia, Sept 23, 2009.Image:Dust Storm in Eastern Washington.jpg|Dust storm in eastern Washingtonmarker.


See also



Notes

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