Haboob

A haboob (Arabic: هَبوب‎ "strong wind") is a type of intense duststorm carried on an atmospheric gravity current. Haboobs are regularly observed in arid regions throughout the world. 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.[1] 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 the sand and debris reaching several kilometers into the sky and leaving up to a foot of sand covering everything in its path. The arid and semiarid regions of North America – in fact, any dryland region – may experience haboobs. In the USA, they are frequently observed in the deserts of Arizona, including Yuma and Phoenix,[2][3] as well as New Mexico and Texas.[4] During thunderstorm formation, winds move in a direction opposite to the storm's travel, and they will 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.[5][6][7]

When this downdraft, or "downburst", reaches the ground, dry, loose sand from the desert settings is essentially blown up, creating a wall of sediment preceding the storm cloud. This wall of sand can be up to 100 km (62 mi) wide and several kilometers in elevation. At their strongest, haboob winds can often travel at 35–100 km/h (~20–60 mph), and they may approach with little to no warning. Often rain is not seen at the ground level as it evaporates in the hot, dry air (a phenomenon known as virga), though on occasion when the rain does persist, the precipitation can contain a considerable quantity of dust (severe cases called "mud storms"). Eye and respiratory system protection are advisable for anyone who must be outside during a haboob—moving to a place of shelter is highly desirable during a strong event.

See also

References

  1. ^ Sutton, L.J. 1925. Haboobs. Quarterly Journal of the Royal Meteorological Society 51:25–25.
  2. ^ Idso, S.B., Ingram, R.S. and Pritchard, J.M. 1972. An American haboob. Bulletin of the American Meteorological Society 53(10):930–955.
  3. ^ Idso, S.B. 1973. Haboobs in Arizona. Weather 28(4):154–155.
  4. ^ Chen, W., and Fryrear, D.W. 2002. Sedimentary characteristics of a haboob dust storm. Atmospheric Research 61(1):75–85.
  5. ^ Farquharson, J.S. 1937. Haboobs and instability in the Sudan. Quarterly Journal of the Royal Meteorological Society 63(271):393–414.
  6. ^ Lawson, T.J. 1971. Haboob structure at Khartoum. Weather 26(3):105–112.
  7. ^ Membery, D.A. 1985. A gravity-wave haboob? Weather 40(7):214–221.

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