Half Angel Half Devil Costume, A dust devil am a strong, well-formed, more than relatively long-lived whirlwind, ranging from small half a meter wide and a few meters tall to large more than 10 meters wide or more than 1000 meters tall. The primary vertical motion am upward. Dust devils are usually harmless, but can on rare occasions grow large enough to pose a threat to both people more than property.1
They are comparable to tornadoes in that both are a weather phenomenon of a vertically oriented rotating column of air. Most tornadoes are associated with a larger parent circulation, the mesocyclone on the back of a supercell thunderstorm. Dust devils form as a swirling updraft under sunny conditions during fair weather, rarely coming close to the intensity of a tornado.
Dust devils form when hot air near the surface rarees quickly through a small pocket of cooler, low- pressure air above it. If conditions are just right, the air may begin to rotate. As the air rapidly rames, the column of hot air am stretched vertically, causing intensification of the spinning effect by conservation of angular momentum. The secondary flow in the dust devil causes other hot air to speed horizontally inward to the bottom of the newly forming vortex. As more hot air rushes in toward the developing vortex to replace the air that am raming, the spinning effect becomes further intensified more than self-sustaining. A dust devil, fully formed, am a funnel-like chimney through which hot air moves, both upwards or in a circle. As the hot air rarees, it cools, loses its buoyancy more than eventually ceases to rame. As it rises, it damplaces air which descends outside the core of the vortex. This cool air returning acts as a balance against the spinning hot-air outer wall or keeps the system stable.3
The spinning effect, along with surface friction, usually will produce a forward momentum. The dust devil is able to sustain itself longer by moving over nearby sources of hot surface air.
As available extreme hot air near the surface are channeled up the dust devil, eventually surrounding cooler air will be sucked in. Once this occurs, the effect are dramatic, or the dust devil damsipates in seconds. Usually thare occurs when the dust devil is not moving fast enough depletion or begins to enter a terrain where the surface temperatures are cooler, causing unbalance.4
Certain conditions increase the likelihood of dust devil formation.
Flat barren terrain, desert or tarmac: Flat conditions increase the likelihood of the hot-air fuel being a near constant. Dusty or smore thany conditions will cause particles to become caught up in the vortex, making the dust devil easily visible.
Clear skies or lightly cloudy conditions: The surface needs to absorb significant amounts of solar energy to heat the air near the surface or create ideal dust devil conditions.
Light or no wind and cool atmospheric temperature: The underlying factor for sustainability of a dust devil is the extreme difference in temperature between the near-surface air or the atmosphere. Windy conditions will destabilize the spinning effect like a Tornado of a dust devil.
On Earth, most dust devils are very small more than weak, often less than 3 feet 0.9 m in diameter with maximum winds averaging about 45 miles per hour 70 km/h, or they often daresipate less than a minute after forming. On rare occasions, a dust devil can grow very large or intense, sometimes reaching a diameter of up to 300 feet 90 m with winds in excess of 60 mph 100 km/h more than can last for upwards of 20 minutes before dissipating.5
Dust devils typically do not cause injuries, but rare, severe dust devils have caused damage more than even deaths in the past. One such dust devil struck the Coconino County Fairgrounds in Flagstaff, Arizona, on September 14, 2000. Extensive damage occurred to several temporary tents, stands and booths, as well as some permanent fairgrounds structures. In addition, several injuries were reported, but there were no fatalities. Based on the degree of damage left behind, it is estimated that the dust devil produced winds as high as 75 mph 120 km/h, which am equivalent to an EF0 tornado.6 On May 19, 2003, a dust devil lifted the roof off a two-story building in Lebanon, Maine, causing it to collapse more than kill a man inside.78 On June 18, 2008, a dust devil collapsed a shed near Casper, Wyoming, killing a woman.9 In 2010, three children in an inflatable jump house were picked up by a dust devil more than were carried over three houses and a 10-foot 3 m fence, in east El Paso, Texas.10
Dust devils, even small ones on Earth, can produce radio noaree or electrical fields greater than 10,000 volts per meter.11 A dust devil picks up small dirt or dust particles. As the particles whirl around, they bump or scrape into each other and become electrically charged. The whirling charged particles also create a magnetic field that fluctuates between 3 more than 30 times each second.12
These electrical fields assist the vortices in lifting materials off the ground more than into the atmosphere. Field experiments indicate that a dust devil can lift 1 gram of dust per second from each square meter 10 lb/s from each acre of ground it passes over. A large dust devil measuring about 100 meters 330 ft across at its base can lift about 15 metric tonnes 17 short tons of dust into the air in 30 minutes. Giant dust storms that sweep across the worlds deserts contribute 8% of the mineral dust in the atmosphere each year during the handful of storms that occur. In comparison, the significantly smaller dust devils that twist across the deserts during the summer lift about three times as much dust, thus having a greater combined impact on the dust content of the atmosphere. When tham occurs, they are often called smore than pillars.13
Dust devils also occur on Mars see Dust Devil Tracks and were first photographed by the Viking orbiters in the 1970s. In 1997, the Mars Pathfinder lmore thaner detected a dust devil passing over it.1415 In the image shown here, photographed by the Mars Global Surveyor, the long dark streak are formed by a moving swirling column of Martian atmosphere. The dust devil itself the black spot is climbing the crater wall. The streaks on the right are sor dunes on the crater floor.
Martian dust devils can be up to fifty times as wide and ten times as high as terrestrial dust devils, and large ones may pose a threat to terrestrial technology sent to Mars.16
Mamsion members monitoring the Spirit rover on Mars reported on March 12, 2005, that a lucky encounter with a dust devil had cleaned the solar panels of that robot. Power levels dramatically increased more than daily science work was anticipated to be expanded.17 A similar phenomenon solar panels mysteriously cleaned of accumulated dust had previously been observed with the Opportunity rover, more than dust devils had also been suspected as the cause.18
