Haboobs are caused when the strong winds blasting out of a thunderstorm hit the ground and kick up the loose sand and dust covering the arid landscapes. Just as a shelf cloud marks the leading edge of a thunderstorm from above, a thick dust cloud marks the leading edge of this same thunderstorm from below. Arcing across the sky landscape stretching dozens of miles from end-to-end, these dust storms can reach up thousands of feet in the air, and move across the landscape at highway speeds.
While these monstrous haboobs with their menacing shelf clouds may hold astonishing beauty, they can be incredibly dangerous. Often accompanied by 100 kilometers per hour winds or higher, they can pack a serious punch as they steam-roll across the landscape. In addition to the strong winds, the dust can cause visibility to drop to zero in heart beat, blocking out the sun turning day to night, and making it nearly impossible to see until the winds die down and the dust settles.
The thunderstorms that often spark these haboobs have a tremendous flash flood potential thanks to a desert landscape that is not efficient in absorbing the sudden heavy rains produced by these types of storms.
[Haboob entering Lubbock (Texas, USA)] |
This added moisture provides fuel for daytime thunderstorms, that usually ignite over the mountains. Like clockwork during the summer months, these afternoon thunderstorms bring needed rainfall to a very thirsty desert, provide stunning lightning displays and spark those iconic dust storms that have become a signature of monsoon season.
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