They have been observed in the Sahara desert (typically Sudan, where they were named and described), as well as across the Arabian Peninsula, throughout Kuwait, and in the most arid regions of Iraq. African haboobs result from the northward summer shift of the inter-tropical front into North Africa, bringing moisture from the Gulf of Guinea. Haboob winds in the Arabian Peninsula, Iraq, Kuwait, and North America are frequently created by the collapse of a thunderstorm, while haboobs in Australia may be frequently associated with cold fronts. The deserts of Central Australia, especially near Alice Springs, are particularly prone to haboobs, with sand and debris reaching several kilometers into the sky and leaving up to 30 centimetres (1 ft) of sand in the haboob's path.
The arid and semiarid regions of North America—in fact, any dry region—may experience haboobs. In North America the most common terms for these events is either dust storm or sandstorm. In the U.S., they frequently occur in the deserts of Arizona, including around the cities of Yuma and Phoenix; in New Mexico, including Albuquerque; and in Texas. During thunderstorm formation, winds move in a direction opposite to the storm's travel, and they move from all directions into the thunderstorm. When the storm collapses and begins to release precipitation, wind directions reverse, gusting outward from the storm and generally gusting the strongest in the direction of the storm's travel. In the Canadian province of Alberta, dust bowls, haboobs and dust storms can commonly occur in the southeastern part of the province, which has a relatively low population but can create severe storms as a result of the clashing events of both a dust storm and Chinook. Because of their strength, the dust storms occasionally enter the boundaries of cities like Calgary, Red Deer, and less commonly Edmonton.
When this downdraft of cold air, or downburst, reaches the ground, it blows dry, loose silt and clay (collectively, dust) up from the desert, creating a wall of sediment that precedes the storm cloud. This wall of dust can be up to 100 km (62 mi) wide and several kilometers in elevation. At their strongest, haboob winds often travel at 35–100 km/h (22–62 mph), and they may approach with little or no warning. Often rain does not appear at ground level as it evaporates in the hot, dry air (a phenomenon known as virga). The evaporation cools the rushing air even further and accelerates it. Occasionally, when the rain does persist, it can contain a considerable quantity of dust. Severe cases are called mud storms. Eye and respiratory system protection are advisable for anyone who must be outside during a haboob. Moving to shelter is highly desirable during a strong event.
A haboob heads into Albuquerque, summer 2013.
A haboob closes in on Nyala Airport
Haboob blowing into Ahwatukee, Phoenix, Arizona, on 22 August 2003.
A haboob approaches Taji, Iraq, in 2006.
A haboob hits the South-East Valley, Gilbert, AZ, USA, on 5 July 2011, around 7 p.m., hiding San Tan Mountain completely.
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|Wikimedia Commons has media related to Haboobs.|
- Haboob Photos @ HikeArizona.COM
- Haboobs, Arizona Department of Transportation.
- The Bibliography of Aeolian Research
- Haboob on Winds of the World
- Short Video of the 5 July 2011 Arizona Haboob (Flash Video software or a web browser supporting H.264/MPEG-4 AVC is necessary to see the content) on YouTube
- Time-lapse video of the 5 July 2011 Arizona Haboob