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Sumatra squall

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seven squalls a month, and slightly less frequently during the southwest monsoon (June–September), with an average of six a month. In comparison, approximately 2.5 squalls per month are observed during the northeast monsoon from December to March. Sumatra squalls observe a clear diurnal pattern and are much more likely to occur in the predawn hours (12 a.m. to 6 a.m.
125:, killing four and damaging 56 houses and 36 schools. Fallen trees and power outages were also reported. In the evening of 17 September 2024, a Sumatra squall felled several trees across Singapore, damaging vehicles and blocking roads. Loose items were flung around by winds gusting up to 83.2 km/h (51.7 mph), and a glass roof at 211:
The mechanisms behind the formation and propagation of Sumatra squalls are not well understood, as observations are sparse and there is thus little data to work with. Several hypotheses exist to explain the development of the initial convective cells that later form the Sumatra squall: heating of air
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A 2016 paper by Lo and Orton used data on 1,337 Sumatra squalls affecting Singapore from January 1988 to December 2009 to compile a climatology of Sumatra squalls. They found that Sumatra squalls occur most commonly during the inter-monsoon periods (April–May and October–November) with an average of
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below the front-to-rear jet transporting air back to the surface, and a cold pool at the surface just behind the leading edge. The Sumatra squall then moves eastwards and grows in size and intensity over the Straits of Malacca, driven by the formation of new convective cells at the squall's leading
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Typically, Sumatra squalls affect Malaysia and Singapore for one to two hours in the night or morning, producing heavy rains along with wind gusts of 40–80 km/h (25–50 mph). The highest recorded wind gust in Singapore—144.4 km/h (89.7 mph) on 25 April 1984, in
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to resolve. Individual forecasters subjectively assessing the outputs of various regional- and global-scale models and analysing real-time observations can have moderately accurate results, though the process is slow and laborious.
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Along the Straits of Malacca, one of the world's most important shipping lanes, the gusty winds of Sumatra squalls make the narrow strait difficult to navigate, which could result in maritime accidents. A letter published in the
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is too insignificant to generate enough rotation. The squall peaks in intensity near or over Malaysia and Singapore, and becomes more diffuse and disorganised after exiting land, eventually dissipating over the South China Sea.
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Ly, Duy Khiem; Tan, Cheng Ann; Ma, Qiang (2016). "Characteristics of Sumatra Squalls and Modelling of the Squall-Generated Waves". In Gourbesville, Philippe; Cunge, Jean A.; Caignaert, Guy (eds.).
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in 1923 noted that boats in the Straits of Malacca were blown ashore by Sumatra squalls. Sumatra squalls are also responsible for significant lightning activity over the strait. The
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Sun, Xiangming; Huang, Xiang-Yu; Gordon, Chris; Mittermaier, Marion; Beckett, Rebecca; Cheong, Wee Kiong; Barker, Dale; North, Rachel; Semple, Allison (1 April 2019).
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below an altitude of 4 km (2.5 mi) and easterlies above that, is necessary for the individual cells to organise into and persist as a squall line.
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Accurately predicting the development of Sumatra squalls is difficult as the relatively small size of Sumatra squalls make them difficult for conventional
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and inter-monsoon periods when the prevailing winds have a greater westerly component. The passage of Sumatra squalls can result in fallen trees,
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Beck, Ferdinand; Bárdossy, András; Seidel, Jochen; Müller, Thomas; Fernandez Sanchis, Elvira; Hauser, Andreas (March 2015).
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Yi, Lan; Lim, Hock (2006). "Semi-idealized COAMPS® simulations of Sumatra squall lines: the role of boundary forcing".
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can serve to increase the frequency of Sumatra squalls by shifting the prevailing winds to the west or southwest.
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After the initial development phase, the Sumatra squall behaves as a typical squall line, with a front-to-rear
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A Sumatra squall over Singapore in the evening of 29 July 2022, viewed from the Stadium Riverside Walk in
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He, Shaoneng; Goodkin, Nathalie F.; Kurita, Naoyuki; Wang, Xianfeng; Rubin, Charles Martin (16 April 2018).
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Chan, Man Yau; Lo, Jeff Chun‐Fung; Orton, Thomas (May 2019). "The structure of tropical Sumatra squalls".
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associated with squalls can pose a risk to nearby aircraft, especially during landing or takeoff, as the
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over the Western Pacific Ocean and Southeast Asia, resulting in a weaker southwest monsoon. Conversely,
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as it intensifies, but does not evolve further to a comma-shape as the turning effect of the
744: 872: 740: 649: 387: 777:"CNA Explains: What is a Sumatra squall and how did it bring a sudden storm to Singapore?" 8: 221: 69: 876: 753: 728: 653: 459: 391: 824: 665: 533: 405: 65: 1042: 1002: 828: 669: 409: 229: 114: 102: 85: 727:
Ilhamsyah, Y; Koesmaryono, Y; Hidayat, R; Murjaya, J; Nurjaya, I W (February 2017).
1089: 1034: 994: 937: 890: 880: 814: 803:"A Subjective and Objective Evaluation of Model Forecasts of Sumatra Squall Events" 748: 699: 657: 395: 213: 188: 92:, and property damage. Shipping along the Straits of Malacca may also be affected. 1072: 1101: 998: 252: 192: 609:"ST Explains: What's a Sumatra squall, and how does it affect S'pore's weather?" 583:"Strong winds, heavy rain batter Singapore, uprooting trees and slowing traffic" 1077: 1038: 942: 925: 861:"Stable Isotopes of Precipitation During Tropical Sumatra Squalls in Singapore" 265: 225: 106: 1111: 1027:
Advances in Geosciences: Solid Earth, Ocean Science & Atmospheric Science
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parcels at the surface by the warm waters of the Straits of Malacca,
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edge (and not by the prevailing winds). The squall forms a
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generated by air flowing down the eastern slopes of the
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events may result in more frequent Sumatra squalls. The
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IOP Conference Series: Earth and Environmental Science
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Quarterly Journal of the Royal Meteorological Society
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from the east coast of Sumatra and the west coast of
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years, such as 1997 and 2015. This is due to reduced
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Quarterly Journal of the Royal Meteorological Society
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Meteorological Service Singapore. 774: 580: 13: 344:Bevan, Simon (14 September 2020). 283: 171:Fewer squalls are observed during 14: 1144: 581:Lee, Elaine (18 September 2024). 452: 433:Rashith, Rahimah (1 April 2018). 334: 297:from the original on 20 July 2021 291:"Weather Systems: Sumatra Squall" 119:Singapore Institute of Management 16:Squall line in Sumatra, Indonesia 1095: 1083: 1071: 949: 909: 841: 760: 686:Benest, E. E. (15 August 2007). 251:at the squall's leading edge, a 147:becomes challenging to control. 957: 917: 794: 768: 720: 679: 600: 574: 548: 993:. Springer. pp. 157–174. 526: 500: 474: 426: 309: 1: 1118:Severe weather and convection 754:10.1088/1755-1315/56/1/012010 460:"Fenomena Cuaca: Garis Badai" 276: 198: 113:and along a slip road on the 64:and moves eastwards over the 999:10.1007/978-981-287-615-7_11 158: 44:(plural: Sumatra squalls or 7: 10: 1149: 1133:Weather events in Malaysia 1039:10.1142/9789812708946_0009 943:10.1016/j.ejrh.2015.02.001 95: 20: 247:characterised by intense 185:Madden–Julian oscillation 56:—that develops over the 1054:(subscription required) 1014:(subscription required) 820:10.1175/WAF-D-19-0187.1 807:Weather and Forecasting 745:2017E&ES...56a2010I 716:(subscription required) 675:(subscription required) 462:(in Malay). MetMalaysia 422:(subscription required) 317:"Weatherwise Singapore" 1128:Geography of Singapore 704:10.1002/qj.49704920807 534:"Fenomena Garis Badai" 208: 37: 206: 31: 886:10.1002/2017JD027829 877:2018JGRD..123.3812H 654:2019Wthr...74..176C 562:. 18 September 2018 392:2016Wthr...71..175L 222:Peninsular Malaysia 70:Peninsular Malaysia 209: 66:Straits of Malacca 38: 1008:978-981-287-615-7 613:The Straits Times 587:The Straits Times 513:The Straits Times 439:The Straits Times 230:Barisan Mountains 189:tropical cyclones 115:Kranji Expressway 86:southwest monsoon 1140: 1100: 1099: 1098: 1088: 1087: 1086: 1076: 1075: 1067: 1056: 1055: 1052: 1022: 1016: 1015: 1012: 986: 980: 979: 977: 975: 969: 961: 955: 954: 953: 947: 945: 921: 915: 914: 913: 907: 905: 903: 898: 888: 871:(7): 3812–3829. 856: 847: 846: 845: 839: 837: 835: 822: 798: 792: 791: 789: 787: 781:Channel NewsAsia 772: 766: 765: 764: 758: 756: 724: 718: 717: 714: 712: 710: 698:(208): 237–238. 683: 677: 676: 673: 662:10.1002/wea.3375 637: 624: 623: 621: 619: 604: 598: 597: 595: 593: 578: 572: 571: 569: 567: 552: 546: 545: 543: 541: 530: 524: 523: 521: 519: 504: 498: 497: 495: 493: 478: 472: 471: 469: 467: 456: 450: 449: 447: 445: 430: 424: 423: 420: 418: 416: 403: 401:10.1002/wea.2748 371: 358: 357: 355: 353: 341: 332: 331: 329: 327: 321: 313: 307: 306: 304: 302: 287: 1148: 1147: 1143: 1142: 1141: 1139: 1138: 1137: 1123:Weather hazards 1108: 1107: 1106: 1096: 1094: 1084: 1082: 1070: 1062: 1060: 1059: 1053: 1049: 1023: 1019: 1013: 1009: 987: 983: 973: 971: 967: 963: 962: 958: 948: 922: 918: 908: 901: 899: 857: 850: 840: 833: 831: 799: 795: 785: 783: 773: 769: 759: 725: 721: 715: 708: 706: 684: 680: 674: 638: 627: 617: 615: 605: 601: 591: 589: 579: 575: 565: 563: 554: 553: 549: 539: 537: 532: 531: 527: 517: 515: 505: 501: 491: 489: 480: 479: 475: 465: 463: 458: 457: 453: 443: 441: 431: 427: 421: 414: 412: 372: 361: 351: 349: 342: 335: 325: 323: 319: 315: 314: 310: 300: 298: 289: 288: 284: 279: 253:rear-inflow jet 201: 193:South China Sea 161: 98: 26: 17: 12: 11: 5: 1146: 1136: 1135: 1130: 1125: 1120: 1105: 1104: 1092: 1080: 1058: 1057: 1047: 1017: 1007: 981: 956: 916: 848: 813:(2): 489–506. 793: 767: 719: 678: 648:(5): 176–181. 625: 599: 573: 547: 525: 499: 488:. 12 June 2014 473: 451: 425: 386:(7): 175–178. 359: 333: 308: 281: 280: 278: 275: 266:Coriolis force 226:mountain waves 200: 197: 160: 157: 152:weather models 107:Seberang Perai 97: 94: 42:Sumatra squall 15: 9: 6: 4: 3: 2: 1145: 1134: 1131: 1129: 1126: 1124: 1121: 1119: 1116: 1115: 1113: 1103: 1093: 1091: 1081: 1079: 1074: 1069: 1068: 1065: 1050: 1048:9789812708946 1044: 1040: 1036: 1032: 1028: 1021: 1010: 1004: 1000: 996: 992: 985: 966: 960: 952: 944: 939: 935: 931: 927: 920: 912: 897: 892: 887: 882: 878: 874: 870: 866: 862: 855: 853: 844: 830: 826: 821: 816: 812: 808: 804: 797: 782: 778: 771: 763: 755: 750: 746: 742: 739:(1): 012010. 738: 734: 730: 723: 705: 701: 697: 693: 689: 682: 671: 667: 663: 659: 655: 651: 647: 643: 636: 634: 632: 630: 614: 610: 603: 588: 584: 577: 561: 557: 551: 535: 529: 514: 510: 503: 487: 483: 477: 461: 455: 440: 436: 429: 411: 407: 402: 397: 393: 389: 385: 381: 377: 370: 368: 366: 364: 348:. StratumFive 347: 340: 338: 318: 312: 296: 292: 286: 282: 274: 271: 267: 263: 262:weather radar 259: 254: 250: 246: 241: 239: 235: 231: 227: 223: 219: 215: 205: 196: 194: 190: 186: 182: 178: 174: 169: 167: 156: 153: 148: 146: 142: 138: 137: 130: 129:was damaged. 128: 124: 120: 116: 112: 108: 104: 93: 91: 87: 83: 79: 75: 71: 67: 63: 59: 55: 54:thunderstorms 51: 47: 43: 35: 30: 24: 19: 1030: 1026: 1020: 990: 984: 972:. Retrieved 959: 933: 929: 919: 900:. Retrieved 868: 864: 832:. Retrieved 810: 806: 796: 786:18 September 784:. Retrieved 780: 770: 736: 732: 722: 707:. Retrieved 695: 691: 681: 645: 641: 618:18 September 616:. Retrieved 612: 602: 592:18 September 590:. Retrieved 586: 576: 566:10 September 564:. Retrieved 559: 550: 540:10 September 538:. Retrieved 528: 516:. Retrieved 512: 502: 490:. Retrieved 485: 476: 464:. Retrieved 454: 442:. Retrieved 438: 428: 413:. Retrieved 383: 379: 350:. Retrieved 324:. Retrieved 311: 299:. 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Index

Sumatra

Kallang
squall line
thunderstorms
Indonesian
Sumatra
Straits of Malacca
Peninsular Malaysia
Singapore
Riau Islands
Indonesia
southwest monsoon
flash floods
Tengah
Seberang Perai
Commonwealth
Kranji Expressway
Singapore Institute of Management
Perlis
UOB Plaza
Quarterly Journal of the Royal Meteorological Society
wind shear
airspeed
weather models
UTC+8
El Niño
convection
La Niña
Madden–Julian oscillation

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