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139:, reaches the ground, it blows dry, loose silt and clay (collectively, dust) up from the desert, creating a wall of airborne 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
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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
333:. In Washington, improved farming practices have led to a decline in large dust storms and haboobs since the 1990s, with the largest likelihood of formation between late March through April, corresponding to the beginning of field tilling in Eastern Washington. In
143:). 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
852:
951:
Rodriguez, S.; Le Mouélic, S.; Barnes, J. W.; Kok, J. F.; Rafkin, S. C. R.; Lorenz, R. D.; Charnay, B.; Radebaugh, J.; Narteau, C.; Cornet, T.; Bourgeois, O. (October 2018).
248:, 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.
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Eye and respiratory system protection is advisable for anyone who must be outside during a haboob. Moving to shelter is highly advised during a strong event.
46:
33:
271:
1039:
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)
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As with haboobs in the Middle East, haboob occurrences in North
America are often created by the collapse of a thunderstorm. This is a local or
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and similar conditions later were in fact synoptic scale events typically generated by a strong cold frontal passage, with storms on
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event, and at times of extreme drought they can originate in agricultural regions. Some of the most famous dust storms of the
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281:—in fact, any dry region—may experience haboobs. In North America, the most common terms for these events are either
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observed in 2009 and 2010 have been compared to haboobs. However, the convective storm clouds are composed of
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853:"Tormenta de arena cubre Guaymas; Protección Civil Sonora emite medidas para la población"
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in the
Arabian Peninsula, Iraq, and Kuwait are frequently created by the collapse of a
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Chen, W.; Fryrear, D.W. (2002). "Sedimentary characteristics of a haboob dust storm".
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855:[Dust storm covers Guaymas; Protección Civil Sonora issues safety measures].
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749:"Photos: Major 'haboob' – dust and windstorm – strikes eastern Washington"
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953:"Observational evidence for active dust storms on Titan at equinox"
775:"Weathercatch: Dust-filled drama of past teaches lesson for future"
496:
Farquharson, J. S. (1937). "Haboobs and instability in the sudan".
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or sandstorm. In the U.S., they frequently occur in the deserts of
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African haboobs result from the northward summer shift of the
180:, where they were named and described), as well as across the
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10.1175/1520-0477(1972)053<0930:AAH>2.0.CO;2
337:, they occur in the northern part of the country in the
827:"What you need to know about dust storms in Washington"
236:
Haboobs in
Australia may be frequently associated with
531:
Lawson, T. J. (1971). "Haboob
Structure at Khartoum".
603:
Quarterly
Journal of the Royal Meteorological Society
498:
Quarterly
Journal of the Royal Meteorological Society
95:
1049:Time-lapse video of the 5 July 2011 Arizona Haboob
636:Idso, S.B.; Ingram, R.S.; Pritchard, J.M. (1972).
107:'blasting/drifting') is a type of intense
566:Membery, D. A. (1985). "A Gravity-Wave Haboob?".
345:. Most recently, a haboob impacted the cities of
677:Idso, Carolyn W. (1973). "Haboobs in Arizona".
642:Bulletin of the American Meteorological Society
1016:Haboobs, Arizona Department of Transportation.
388:, and the dust is likely composed of organic
8:
773:Loyd, Nic; Weiford, Linda (12 August 2021).
881:. FiveThirtyEight. Retrieved 9 March 2017.
916:
831:Department of Ecology State of Washington
805:Department of Ecology State of Washington
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372:have been compared to haboobs on Earth.
49:of all important aspects of the article.
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315:Washington State Department of Ecology
45:Please consider expanding the lead to
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944:
7:
1028:The Bibliography of Aeolian Research
891:Keane, James Tuttle (October 2018).
879:"Everything About Mars Is the Worst"
135:When this downdraft of cold air, or
747:Ellison, Jake (18 September 2013).
85:
699:10.1002/j.1477-8696.1973.tb02253.x
588:10.1002/j.1477-8696.1985.tb06877.x
553:10.1002/j.1477-8696.1971.tb07402.x
188:, and in the most arid regions of
168:Haboobs have been observed in the
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601:Sutton, L. J. (1925). "Haboobs".
289:, including around the cities of
277:The arid and semiarid regions of
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325:, and can impact cities such as
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801:"Get ready, it's haboob season"
37:may be too short to adequately
434:Intertropical Convergence Zone
218:Intertropical Convergence Zone
212:Small boat in River Nile Sudan
119:regions throughout the world.
115:. Haboobs occur regularly in
47:provide an accessible overview
1:
734:10.1016/S0169-8095(01)00092-8
224:, bringing moisture from the
123:Formation and characteristics
1033:Haboob on Winds of the World
851:Grupo Healy (20 July 2023).
825:Vaughn, Kim (1 April 2021).
799:Vaughn, Kim (1 April 2021).
96:
72:Haboob in Big Spring, Texas
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877:Boyle, R. (9 March 2017).
370:Global dust storms on Mars
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16:Type of intense dust storm
977:10.1038/s41561-018-0233-2
918:10.1038/s41561-018-0240-3
317:, they also occur in the
111:carried by the wind of a
484:Encyclopædia Britannica
386:liquid methane droplets
623:10.1002/qj.49705121305
518:10.1002/qj.49706327111
258:North American Monsoon
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1021:8 August 2013 at the
272:11 November 1911
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71:
779:The Spokesman-Review
714:Atmospheric Research
638:"An American Haboob"
132:the storm's travel.
969:2018NatGe..11..727R
909:2018NatGe..11..705K
726:2002AtmRe..61...75C
691:1973Wthr...28..154I
654:1972BAMS...53..930I
615:1925QJRMS..51...25S
580:1985Wthr...40..214M
545:1971Wthr...26..105L
510:1937QJRMS..63..393F
893:"Haboobs on Titan"
323:Eastern Washington
244:, especially near
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74:
1012:@ HikeArizona.COM
957:Nature Geoscience
897:Nature Geoscience
361:on 20 July 2023.
343:Chihuahuan Desert
242:Central Australia
240:. The deserts of
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55:September 2023
41:the key points
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861:. Retrieved
859:(in Spanish)
857:El Imparcial
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198:thunderstorm
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129:thunderstorm
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34:lead section
1064:Dust storms
903:(10): 705.
419:Bora (wind)
327:Walla Walla
303:Albuquerque
238:cold fronts
176:(typically
164:Middle East
1058:Categories
753:Seattle PI
466:References
429:Dust devil
351:San Carlos
313:. Per the
307:California
305:; eastern
299:New Mexico
283:dust storm
256:See also:
159:Occurrence
145:mud storms
109:dust storm
993:134006536
985:1752-0908
935:135135003
927:1752-0908
268:Dust Bowl
264:mesoscale
232:Australia
192:. Haboob
137:downburst
91:romanized
39:summarize
1019:Archived
396:See also
1044:YouTube
965:Bibcode
905:Bibcode
863:21 July
836:22 June
810:22 June
784:22 June
758:22 June
722:Bibcode
687:Bibcode
679:Weather
650:Bibcode
611:Bibcode
576:Bibcode
568:Weather
541:Bibcode
533:Weather
506:Bibcode
481:at the
459:Sirocco
439:Khamsin
390:tholins
355:Empalme
347:Guaymas
339:Sonoran
331:Spokane
295:Phoenix
287:Arizona
127:During
105:
93::
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983:
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479:Haboob
454:Simoom
359:Sonora
353:, and
335:Mexico
309:; and
186:Kuwait
170:Sahara
151:Safety
82:Arabic
78:haboob
1069:Storm
989:S2CID
931:S2CID
382:Titan
376:Titan
311:Texas
297:; in
220:into
194:winds
178:Sudan
174:Sahel
141:virga
97:habūb
86:هَبوب
981:ISSN
923:ISSN
865:2023
838:2023
812:2023
786:2023
760:2023
365:Mars
341:and
329:and
293:and
291:Yuma
190:Iraq
103:lit.
1042:on
973:doi
913:doi
730:doi
695:doi
658:doi
619:doi
584:doi
549:doi
514:doi
321:of
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