Knowledge (XXG)

Alpine storms

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fingers (...) A pendulum swing puts me near Pierrot, when a flash of a surprising glow hits him in the face, exactly in the ear where his hearing aid blackens. He falls into my arms, haggard, disgusted, without reaction". He also noted that Pierre Kohlmann was not killed instantly but the shock seemed to make him lose his mind. During the several days that it took to descend, he did not say a word, finally collapsing just before reaching the entrance, the last victim of the storm that killed four mountaineers.
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In a more general case, several effects may be present and if the synoptic wind is opposed to the anabatic wind, additional convergence occurs at the top of the mountain. It is also possible to create a convergence zone behind the mountain when the synoptic wind can divide and go around it to meet
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Thunderstorms are formed when air in a layer of the atmosphere is unstable. A parcel of air raised at the base of this layer is then warmer than the environment and rises. In rising, its temperature decreases by adiabatic expansion, and when the relative humidity of water vapor reaches saturation,
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About the 1961 disaster, Mazeaud wrote: "Sitting on my stirrups, I use my piton, when I hear a striking ring somewhat resembling the phone. My companions, forty meters below, prick up their ears. Soon, I feel pain in my fingers, sparks run on my hammer. The carabiners on my shoulder stick to my
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of the air. French mountaineers say they hear "bees": suddenly, on all surfaces, are small noisy discharges. After this bee-sound, another observation is that the hair stands straight up over the head, and sparks can form between the teeth when one opens one's mouth. These are the results of
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Mountain storms have particularities because of the proximity of clouds, the importance of electric fields, their rapidity of appearance, their particular danger. Sudden wind lift of a mass of air can radically change the initial conditions within them.
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when air is stable lower down, and circulation is blocked by the mountain, but the air is unstable at higher altitude. In this case general circulation is forced above this blocking layer and can reach the convective
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The uprising serves to not only destabilize the air and form convective clouds, but also to enhance its intensity. As the rising air from the bottom of the slopes is hotter and humid than the surrounding air, the
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on July 11, 1961, where seven mountaineers were surprised by a violent storm on the pillar of FrĂȘney, near the summit of Mont Blanc. One hundred and ten hours later, a helicopter landed three survivors at
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and paragliders. Despite monitoring weather conditions to prevent accidents, disasters occurring during such phenomena often remain unpredictable and are the subject of novels or other stories.
302:) by Roger Frison-Roche touched on the spectacle of mountain climbing and the experience of high mountain guides in these extreme situations. It was adapted to the cinema in a 1944 film by 76:
at the level of free convection in unstable air, lifting with a synoptic wind that arrives w/ a component perpendicular to the slopes. The air is forced up the slope and into convection;
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will be more negative, increasing the vertical extension of the cloud . A simple temperature difference of 2C is enough to greatly aggravate the violence of thunderstorms.
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Climbers, not very mobile, can find themselves trapped in a storm. The metal ice axes of climbing equipment can attract lightning, a great danger in these situations.
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Formation of a cold front when the air in an uplift is stable or can not reach the top of the obstacle. The air is forced over the front and causes the formation of a
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is an essential tool for preventing accidents related to mountain storms but does not prevent them. Climbers must know how to respond to a storm in the mountains.
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said: "I have often bivouacked to wait for the good weather, spent nights in the storm ... In a storm, there is nothing to do but sit, wait for it to pass... ".
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provides forecasts for every point in its territory, including the mountainous areas. In other countries, similar services and guidance are provided by the
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this forms a convective cloud. To form a storm, this layer must be very large and the temperature at the top of the cloud must be below −20C.
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A number of mountaineers in the 20th century wrote autobiographical accounts of being caught in mountain storms.
1109: 260: 224:, bursts and whirlwinds can cause other dangerous situations. Some natural phenomena are increased tenfold by 544:"Les orages — CultureSciences-Physique - Ressources scientifiques pour l'enseignement des sciences physiques" 543: 471:
Contribution d'un code de calcul météorologique méso-échelle à la climatologie des pluies en zone de relief
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in France. France also maintains a Safe Mountain Foundation and Keraunos, an observatory for
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in an unstable situation where there is weak general circulation and diurnal warming. The
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electrical phenomena, already described in other situations, and known by the name of
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Mountaineers are the most exposed to these phenomena, in ridges and pass passes.
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again (ex. Puget Sound Convergence Zone ) that will promote convection.
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pose significant risks because of their consequences, especially for
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Cotton, William R; Bryan, George H; van den Heever, Susan C (2011).
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Observable phenomena give an idea of the peculiarities of mountain
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In addition to the common phenomena related to the storm, larger
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Cumulonimbus rising above the Black Mountains (North Carolina).
477:. ThĂšse de J. Vetter. Cemagref. pp. 17–21. Archived from 773: 750:"Conditions montagne gĂ©nĂ©rales, alpinisme, cascades, ski" 503: 915:"[Association Pierre Kohlmann] Pierre Kohlmann" 800:
Les horizons lointains: Souvenirs d'une vie d'alpiniste
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Thillet, Jean-Jacques; Schueller, Dominique (2009).
938:: CS1 maint: bot: original URL status unknown ( 736: 597: 1031:. Éditions du Chemin des CrĂȘtes. p. 208. 147:cause unexpected warning signs related to the 232:torrential floods down slopes at rapid speeds 86:then generate anabatic winds which also rise. 8: 572:"Revue PyrĂ©nĂ©enne : Orages en Montagne" 156:or corona effect also called crown effect. 921:. Archived from the original on 2013-07-02 283:Stories of mountain storms in literature 504:Cotton, Bryan & van den Heever 2011 463: 461: 422: 931: 888:"Il y a 50 ans, la tragĂ©die du FrĂȘney" 548:Science Resources for Teaching Physics 7: 986:. Topo guides. GlĂ©nat. p. 192. 637: 635: 633: 631: 430: 428: 426: 363:. This book reports the tragedy on 681:"Petit manuel de mĂ©tĂ©o de montagne" 14: 342:: Surprised during the ascent of 754:www.fondazionemontagnasicura.org 265:Meteorological Service of Canada 797:Bonington, Chris (2013-07-15). 359:(Mountain for a naked man), by 984:Petit manuel de mĂ©tĂ©o montagne 570:Joseph, F. (1 December 1985). 468:Vetter, Julien (5 July 2004). 1: 1087:The Conquerors of the Useless 336:The Conquerors of the useless 737:Thillet & Schueller 2009 598:Thillet & Schueller 2009 440:Glossaire de la mĂ©tĂ©orologie 615:www.techniques-ingenieur.fr 349:The famous British climber 65:Mountains can help trigger 1131: 708:"QUE FAIRE EN CAS D'ORAGE" 648:Revue de gĂ©ographie alpine 259:In the United States, the 166: 122: 42: 1051:Montagne pour un homme nu 1029:Parapente Vol de distance 894:(in French). 17 July 2011 578:(in French). pp. 4–6 550:(in French). 12 June 2003 357:Montagne pour un homme nu 1053:. Arthaud. p. 304. 1027:Dominique Musto (2014). 1003:Storm and Cloud Dynamics 712:www.clubalpin-tarbes.org 642:Chardon, Michel (1989). 261:National Weather Service 181:Torrential flood in the 803:(in French). Primento. 687:(in French). 2015-09-05 576:French National Library 523:(in French). June 2015 328: 327:Walter Bonatti in 1965 205: 190: 119:Immediate consequences 67:atmospheric convection 58: 25:Mountain thunderstorms 21: 660:10.3406/rga.1989.2727 326: 196: 180: 163:Indirect consequences 52: 19: 417:Notes and references 55:low level jet stream 1069:Mountains of a life 862:Montagnes d'une vie 254:Weather forecasting 959:www.summitpost.org 892:Le DauphinĂ© LibĂ©rĂ© 484:on 29 October 2015 329: 206: 191: 59: 22: 401:Saint Elmo's fire 300:First on the Rope 295:Premier de cordĂ©e 228:, in particular: 110:Special phenomena 1122: 1067:Walter Bonatti, 1064: 1042: 1016: 1012:978-0-12-0885428 997: 969: 968: 966: 965: 951: 945: 943: 937: 929: 927: 926: 911: 905: 903: 901: 899: 884: 878: 876: 853: 847: 828: 822: 820: 818: 817: 794: 788: 787: 785: 784: 778:www.keraunos.org 770: 764: 763: 761: 760: 746: 740: 734: 728: 726: 724: 723: 714:. Archived from 706:Champetier, JL. 703: 697: 695: 693: 692: 677: 671: 669: 667: 666: 639: 626: 624: 622: 621: 607: 601: 595: 589: 587: 585: 583: 567: 561: 559: 557: 555: 540: 534: 532: 530: 528: 513: 507: 501: 495: 493: 491: 489: 483: 476: 465: 456: 455: 453: 451: 432: 406:Corona discharge 312:Edouard Niermans 154:fire of St. Elmo 129:Corona discharge 84:mountain breezes 1130: 1129: 1125: 1124: 1123: 1121: 1120: 1119: 1110:Montane ecology 1100: 1099: 1085:Lionel Terray, 1075:, 1997, 401 p. 1061: 1045: 1039: 1038:9-782953-919141 1026: 1023: 1021:Further reading 1013: 1000: 994: 981: 978: 973: 972: 963: 961: 953: 952: 948: 930: 924: 922: 913: 912: 908: 897: 895: 886: 885: 881: 873: 855: 854: 850: 829: 825: 815: 813: 811: 796: 795: 791: 782: 780: 772: 771: 767: 758: 756: 748: 747: 743: 735: 731: 721: 719: 705: 704: 700: 690: 688: 679: 678: 674: 664: 662: 641: 640: 629: 619: 617: 609: 608: 604: 596: 592: 581: 579: 569: 568: 564: 553: 551: 542: 541: 537: 526: 524: 515: 514: 510: 502: 498: 487: 485: 481: 474: 467: 466: 459: 449: 447: 434: 433: 424: 419: 387: 351:Chris Bonington 321: 319:Autobiographies 290: 285: 251: 175: 173:Torrential rain 165: 145:electric fields 131: 125:St. Elmo's fire 121: 112: 90:dynamic forcing 80:thermal forcing 69:in three ways: 47: 41: 12: 11: 5: 1128: 1126: 1118: 1117: 1112: 1102: 1101: 1098: 1097: 1083: 1065: 1060:978-2070733415 1059: 1047:Pierre Mazeaud 1043: 1037: 1022: 1019: 1018: 1017: 1011: 998: 993:978-2723463195 992: 977: 974: 971: 970: 946: 906: 879: 871: 857:Walter Bonatti 848: 830:1971 Arthaud, 823: 809: 789: 765: 741: 729: 698: 685:Le Guide MĂ©tĂ©o 672: 627: 602: 590: 562: 535: 508: 496: 457: 436:"Cumulonimbus" 421: 420: 418: 415: 414: 413: 408: 403: 398: 396:Severe weather 393: 386: 383: 378: 377: 374:Walter Bonatti 361:Pierre Mazeaud 354: 347: 320: 317: 316: 315: 308:Maurice Baquet 289: 286: 284: 281: 277:violent storms 250: 247: 246: 245: 239: 233: 164: 161: 120: 117: 111: 108: 95: 94: 87: 77: 74:direct lifting 40: 37: 13: 10: 9: 6: 4: 3: 2: 1127: 1116: 1113: 1111: 1108: 1107: 1105: 1096: 1092: 1088: 1084: 1082: 1081:2-7003-1144-2 1078: 1074: 1070: 1066: 1062: 1056: 1052: 1048: 1044: 1040: 1034: 1030: 1025: 1024: 1020: 1014: 1008: 1004: 999: 995: 989: 985: 980: 979: 975: 960: 956: 950: 947: 941: 935: 920: 916: 910: 907: 893: 889: 883: 880: 874: 872:2-7003-1144-2 868: 864: 861: 858: 852: 849: 845: 844:9782081313439 841: 837: 833: 827: 824: 812: 810:9782511006566 806: 802: 801: 793: 790: 779: 775: 769: 766: 755: 751: 745: 742: 739:, p. 171 738: 733: 730: 718:on 2016-10-19 717: 713: 709: 702: 699: 686: 682: 676: 673: 661: 657: 653: 649: 645: 638: 636: 634: 632: 628: 616: 612: 606: 603: 600:, p. 111 599: 594: 591: 577: 573: 566: 563: 549: 545: 539: 536: 522: 518: 512: 509: 506:, p. 351 505: 500: 497: 480: 473: 472: 464: 462: 458: 445: 441: 437: 431: 429: 427: 423: 416: 412: 409: 407: 404: 402: 399: 397: 394: 392: 389: 388: 384: 382: 375: 372:; among them 371: 366: 362: 358: 355: 352: 348: 345: 341: 340:Lionel Terray 337: 334: 333: 332: 325: 318: 313: 309: 305: 301: 297: 296: 292: 291: 287: 282: 280: 278: 274: 270: 266: 262: 257: 255: 248: 243: 240: 237: 234: 231: 230: 229: 227: 223: 219: 215: 212:, lightning, 211: 208:The force of 203: 199: 195: 188: 184: 183:canton of Uri 179: 174: 170: 162: 160: 157: 155: 150: 146: 141: 138: 136: 130: 126: 118: 116: 109: 107: 105: 99: 91: 88: 85: 81: 78: 75: 72: 71: 70: 68: 63: 56: 51: 46: 38: 36: 34: 30: 26: 18: 1086: 1068: 1050: 1028: 1002: 983: 976:Bibliography 962:. 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Mazeaud. 964:2023-09-30 925:2016-10-21 919:archive.is 898:21 October 836:208131343X 816:2016-10-22 783:2016-11-01 759:2016-11-01 722:2016-10-19 691:2016-10-19 665:2016-10-19 620:2016-10-19 582:19 October 554:19 October 527:19 October 488:22 October 450:22 October 370:Courmayeur 365:Mont Blanc 269:Met Office 249:Prevention 242:avalanches 236:landslides 167:See also: 149:ionization 123:See also: 43:See also: 654:: 15–28. 411:Avalanche 271:, and by 214:lightning 200:painting 198:Avalanche 169:Avalanche 39:Formation 1049:(1971). 1041:. Musto. 934:cite web 859:(1997). 385:See also 226:altitude 210:thunder 1115:Storms 1093:  1079:  1057:  1035:  1009:  990:  869:  842:  834:  807:  446:. 2009 135:storms 93:layer. 33:hikers 1073:Paris 521:L'Obs 482:(PDF) 475:(PDF) 306:with 288:Novel 1091:ISBN 1077:ISBN 1055:ISBN 1033:ISBN 1007:ISBN 988:ISBN 940:link 900:2016 867:ISBN 840:ISBN 832:ISBN 805:ISBN 584:2016 556:2016 529:2016 490:2016 452:2016 222:hail 218:rain 171:and 127:and 656:doi 338:by 1106:: 957:. 936:}} 932:{{ 917:. 890:. 838:, 776:. 752:. 710:. 683:. 652:77 650:. 646:. 630:^ 613:. 574:. 546:. 519:. 460:^ 442:. 438:. 425:^ 279:. 220:, 216:, 185:, 137:. 31:, 1015:. 996:. 967:. 944:. 942:) 928:. 904:. 902:. 877:. 875:. 821:. 819:. 786:. 762:. 727:. 725:. 696:. 694:. 670:. 668:. 658:: 625:. 623:. 588:. 586:. 560:. 558:. 533:. 531:. 494:. 492:. 454:. 314:. 298:( 244:. 238:, 189:. 57:.

Index


mountaineers
hikers
Thunderstorm

low level jet stream
atmospheric convection
mountain breezes
St. Elmo's fire
Corona discharge
storms
electric fields
ionization
fire of St. Elmo
Avalanche
Torrential rain

canton of Uri
Switzerland

thunder
lightning
rain
hail
altitude
landslides
avalanches
Weather forecasting
National Weather Service
Meteorological Service of Canada

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