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Haboob

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209: 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 404: 69: 25: 131:
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. 155:
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.
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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
433: 217: 826: 318: 281:—in fact, any dry region—may experience haboobs. In North America, the most common terms for these events are either 1043: 483: 38: 1073: 350: 800: 384:
observed in 2009 and 2010 have been compared to haboobs. However, the convective storm clouds are composed of
662: 637: 274:, 9–11 May 1934, 14 April 1935, and 19 February 1954 having been particularly vivid examples. 326: 302: 878: 257: 90: 263: 1063: 964: 904: 721: 686: 649: 610: 575: 540: 505: 403: 102: 988: 930: 322: 980: 922: 342: 241: 181: 972: 912: 729: 694: 657: 618: 583: 548: 513: 448: 423: 385: 294: 1022: 853:"Tormenta de arena cubre Guaymas; Protección Civil Sonora emite medidas para la población" 369: 354: 81: 68: 1032: 968: 908: 725: 690: 653: 614: 579: 544: 509: 1068: 1015: 698: 587: 552: 443: 409: 338: 225: 196:
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".
1057: 992: 934: 855:[Dust storm covers Guaymas; Protección Civil Sonora issues safety measures]. 290: 278: 245: 112: 952: 478: 381: 221: 197: 128: 1027: 418: 1009: 1037: 976: 917: 892: 428: 399: 306: 298: 282: 237: 108: 984: 926: 267: 136: 622: 517: 24: 749:"Photos: Major 'haboob' – dust and windstorm – strikes eastern Washington" 458: 438: 346: 330: 286: 453: 389: 358: 334: 185: 169: 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
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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
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Lawson, T. J. (1971). "Haboob Structure at Khartoum".
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Quarterly Journal of the Royal Meteorological Society
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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 661: 372:have been compared to haboobs on Earth. 49:of all important aspects of the article. 471: 315:Washington State Department of Ecology 45:Please consider expanding the lead to 946: 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 14: 601:Sutton, L. J. (1925). "Haboobs". 289:, including around the cities of 277:The arid and semiarid regions of 402: 325:, and can impact cities such as 23: 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 1092: 877:Boyle, R. (9 March 2017). 370:Global dust storms on Mars 255: 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 213: 73: 1021:8 August 2013 at the 272:11 November 1911 211: 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 214: 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 182:Arabian Peninsula 106: 94: 64: 63: 1081: 1040: 997: 996: 948: 939: 938: 920: 888: 882: 875: 869: 868: 866: 864: 848: 842: 841: 839: 837: 822: 816: 815: 813: 811: 796: 790: 789: 787: 785: 770: 764: 763: 761: 759: 744: 738: 737: 709: 703: 702: 674: 668: 667: 665: 633: 627: 626: 598: 592: 591: 563: 557: 556: 528: 522: 521: 504:(271): 393–414. 493: 487: 476: 449:Outflow boundary 424:Dry thunderstorm 412: 407: 406: 101: 99: 89: 87: 59: 56: 50: 27: 19: 1091: 1090: 1084: 1083: 1082: 1080: 1079: 1078: 1074:Weather hazards 1054: 1053: 1038: 1023:Wayback Machine 1006: 1001: 1000: 963:(10): 727–732. 950: 949: 942: 890: 889: 885: 876: 872: 862: 860: 850: 849: 845: 835: 833: 824: 823: 819: 809: 807: 798: 797: 793: 783: 781: 772: 771: 767: 757: 755: 746: 745: 741: 711: 710: 706: 676: 675: 671: 648:(10): 930–935. 635: 634: 630: 600: 599: 595: 565: 564: 560: 530: 529: 525: 495: 494: 490: 477: 473: 468: 463: 408: 401: 398: 380:Dust storms of 378: 367: 260: 254: 234: 206: 166: 161: 153: 125: 60: 54: 51: 44: 32:This article's 28: 17: 12: 11: 5: 1089: 1088: 1085: 1077: 1076: 1071: 1066: 1056: 1055: 1052: 1051: 1046: 1035: 1030: 1025: 1013: 1005: 1004:External links 1002: 999: 998: 940: 883: 870: 843: 817: 791: 765: 739: 704: 685:(4): 154–155. 669: 628: 609:(213): 25–30. 593: 574:(7): 214–221. 558: 539:(3): 105–112. 523: 488: 470: 469: 467: 464: 462: 461: 456: 451: 446: 444:Mistral (wind) 441: 436: 431: 426: 421: 415: 414: 413: 410:weather portal 397: 394: 377: 374: 366: 363: 319:Columbia Basin 253: 250: 233: 230: 226:Gulf of Guinea 205: 202: 165: 162: 160: 157: 152: 149: 124: 121: 62: 61: 55:September 2023 41:the key points 31: 29: 22: 15: 13: 10: 9: 6: 4: 3: 2: 1087: 1086: 1075: 1072: 1070: 1067: 1065: 1062: 1061: 1059: 1050: 1047: 1045: 1041: 1036: 1034: 1031: 1029: 1026: 1024: 1020: 1017: 1014: 1011: 1010:Haboob Photos 1008: 1007: 1003: 994: 990: 986: 982: 978: 974: 970: 966: 962: 958: 954: 947: 945: 941: 936: 932: 928: 924: 919: 914: 910: 906: 902: 898: 894: 887: 884: 880: 874: 871: 858: 854: 847: 844: 832: 828: 821: 818: 806: 802: 795: 792: 780: 776: 769: 766: 754: 750: 743: 740: 735: 731: 727: 723: 719: 715: 708: 705: 700: 696: 692: 688: 684: 680: 673: 670: 664: 659: 655: 651: 647: 643: 639: 632: 629: 624: 620: 616: 612: 608: 604: 597: 594: 589: 585: 581: 577: 573: 569: 562: 559: 554: 550: 546: 542: 538: 534: 527: 524: 519: 515: 511: 507: 503: 499: 492: 489: 486: 485: 480: 475: 472: 465: 460: 457: 455: 452: 450: 447: 445: 442: 440: 437: 435: 432: 430: 427: 425: 422: 420: 417: 416: 411: 405: 400: 395: 393: 391: 387: 383: 375: 373: 371: 364: 362: 360: 356: 352: 348: 344: 340: 336: 332: 328: 324: 320: 316: 312: 308: 304: 300: 296: 292: 288: 284: 280: 279:North America 275: 273: 269: 265: 259: 252:North America 251: 249: 247: 246:Alice Springs 243: 239: 231: 229: 227: 223: 219: 210: 203: 201: 199: 195: 191: 187: 184:, throughout 183: 179: 175: 171: 163: 158: 156: 150: 148: 146: 142: 138: 133: 130: 122: 120: 118: 117:dry land area 114: 113:weather front 110: 104: 98: 92: 83: 79: 70: 66: 58: 48: 42: 40: 35: 30: 26: 21: 20: 960: 956: 900: 896: 886: 873: 861:. Retrieved 859:(in Spanish) 857:El Imparcial 856: 846: 834:. Retrieved 830: 820: 808:. Retrieved 804: 794: 782:. Retrieved 778: 768: 756:. Retrieved 752: 742: 720:(1): 75–85. 717: 713: 707: 682: 678: 672: 645: 641: 631: 606: 602: 596: 571: 567: 561: 536: 532: 526: 501: 497: 491: 482: 474: 379: 368: 301:, including 276: 261: 235: 222:North Africa 215: 204:North Africa 198:thunderstorm 167: 154: 144: 134: 129:thunderstorm 126: 77: 75: 65: 52: 36: 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::  991:  983:  933:  925:  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 1060:: 987:. 979:. 971:. 961:11 959:. 955:. 943:^ 929:. 921:. 911:. 901:11 899:. 895:. 829:. 803:. 777:. 751:. 728:. 718:61 716:. 693:. 683:28 681:. 656:. 646:53 644:. 640:. 617:. 607:51 605:. 582:. 572:40 570:. 547:. 537:26 535:. 512:. 502:63 500:. 392:. 357:, 349:, 228:. 200:. 172:, 147:. 100:, 88:, 84:: 76:A 995:. 975:: 967:: 937:. 915:: 907:: 867:. 840:. 814:. 788:. 762:. 736:. 732:: 724:: 701:. 697:: 689:: 666:. 660:: 652:: 625:. 621:: 613:: 590:. 586:: 578:: 555:. 551:: 543:: 520:. 516:: 508:: 80:( 57:) 53:( 43:.

Index


lead section
summarize
provide an accessible overview

Arabic
romanized
lit.
dust storm
weather front
dry land area
thunderstorm
downburst
virga
Sahara
Sahel
Sudan
Arabian Peninsula
Kuwait
Iraq
winds
thunderstorm

Intertropical Convergence Zone
North Africa
Gulf of Guinea
cold fronts
Central Australia
Alice Springs
North American Monsoon

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