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| Near Clovis, Photo by Jessica-Marie Barriere |
| Home | Introduction | Flash Floods | Lightning | Downburst WInds | Dust Storms | Heat Stress |
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Dust Storms |
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While downburst winds often do produce local, short-lived areas of blowing dust, larger convective clusters can result in wind spread areas of blowing dust, at times persisting for 30 to 60 minutes. The photos below are from El Paso (left) and Santa Teresa (right) and are examples of more extreme dust storms in southern New Mexico. |
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The most extreme cases of dust storms in New Mexico occur in the extreme southern portions of the state, and are referred to as "haboobs." A haboob is an extreme dust storm that can persist for 1 to 3 hours. The onset of the dust is extreme - it is virtually a wall of dust, as shown in the photos below from near Columbus, NM (left) and El Paso, TX (right). |
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Downburst Wind Safety:
Dust Storm Safety:
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Storm Data has listed 816 thunderstorm wind events as either dry or wet microbursts since 1990. There are likely many other thunderstorm wind events that could be classified as microbursts or macrobursts. Destructive winds up to 70 mph were recently reported near Dora and Floyd on June 7, 2013. On a somewhat larger scale, on August 4, 1998, a line of thunderstorms moving off the San Andres Range produced a macroburst with winds that measured 112 mph at the White Sands Missile Range. The anemometer at Holloman AFB recorded speeds of 75 mph before breaking! The core of strongest winds moved over uninhabited military land, but considerable tree damage and some structural damage occurred well to the east near Alamogordo in Bolles Acres. It was also reported that a vehicle was blown sideways for two blocks. Storm Data also lists a number of dusts storms since 1990. A dust storm in Lordsburg on the 4th of July, 1974 injured 13 people! |
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Downbursts are particularly strong downdrafts from thunderstorms. Downbursts in air that is precipitation free or contains virga are known as dry downbursts; those accompanied with precipitation are known as wet downbursts. Most downbursts are less than 2.5 miles in extent: these are called microbursts. Downbursts larger than 2.5 miles in extent are sometimes called macrobursts. Downbursts can occur over large areas. In the extreme case, a derecho (a widespread and long-lived, violent convectively induced straight-line windstorm that is associated with a fast-moving band of severe thunderstorms in the form of a squall line) can cover a huge area more than 200 miles wide and over 1000 miles long, lasting up to 12 hours or more, and is associated with some of the most intense straight-line winds, but the generative process is somewhat different from that of most downbursts. |
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