Cumulonimbus rising above the Black Mountains (North Carolina).

Mountain thunderstorms pose significant risks because of their consequences, especially for mountaineers, hikers 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.

Formation

See also: Thunderstorm

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 low level jet stream .

Thunderstorms are formed when air in a layer of the atmosphere is unstable.[1] 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, this forms a convective cloud.[1] To form a storm, this layer must be very large and the temperature at the top of the cloud must be below −20C.

Mountains can help trigger atmospheric convection in three ways:[2]

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.[3] It is also possible to create a convergence zone behind the mountain when the synoptic wind can divide and go around it to meet again (ex. Puget Sound Convergence Zone ) that will promote convection.[2]

The uprising serves to not only destabilize the air and form convective clouds, but also to enhance its intensity.[1] As the rising air from the bottom of the slopes is hotter and humid than the surrounding air, the lifted index 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.

Special phenomena

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.

Immediate consequences

See also: St. Elmo's fire and Corona discharge

Observable phenomena give an idea of the peculiarities of mountain storms .

Mountaineers are the most exposed to these phenomena,[4] in ridges and pass passes.

In addition to the common phenomena related to the storm, larger electric fields cause unexpected warning signs related to the ionization of the air.[5] French mountaineers say they hear "bees": suddenly, on all surfaces, are small noisy discharges.[6][7] 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 electrical phenomena, already described in other situations, and known by the name of fire of St. Elmo or corona effect also called crown effect.[8]

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.

Indirect consequences

See also: Avalanche and Torrential rain

Torrential flood in the canton of Uri, Switzerland .
Avalanche painting in the Alps, painted in 1803 by Philippe-Jacques de Loutherbourg .

The force of thunder, lightning, lightning, rain, hail, bursts and whirlwinds can cause other dangerous situations. Some natural phenomena are increased tenfold by altitude,[9] in particular:

Prevention

Weather forecasting is an essential tool for preventing accidents related to mountain storms[10] but does not prevent them. Climbers must know how to respond to a storm in the mountains.[11]

In the United States, the National Weather Service provides forecasts for every point in its territory, including the mountainous areas. In other countries, similar services and guidance are provided by the Meteorological Service of Canada, by the UK Met Office, and by Météo France in France.[12] France also maintains a Safe Mountain Foundation[13] and Keraunos, an observatory for violent storms.[14]

Stories of mountain storms in literature

Novel

Autobiographies

Walter Bonatti in 1965

A number of mountaineers in the 20th century wrote autobiographical accounts of being caught in mountain storms.

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 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[19] 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.[20]

See also

Notes and references

  1. ^ a b c "Cumulonimbus". Glossaire de la météorologie. Météo-France. 2009. Retrieved 22 October 2016.
  2. ^ a b Vetter, Julien (5 July 2004). Contribution d'un code de calcul météorologique méso-échelle à la climatologie des pluies en zone de relief (PDF). Thèse de J. Vetter. Cemagref. pp. 17–21. Archived from the original (PDF) on 29 October 2015. Retrieved 22 October 2016..
  3. ^ Cotton, Bryan & van den Heever 2011, p. 351
  4. ^ "Randonneurs tués dans une coulée de boue en Corse : "On les avait prévenus du risque"". L'Obs (in French). June 2015. Retrieved 19 October 2016..
  5. ^ "Les orages — CultureSciences-Physique - Ressources scientifiques pour l'enseignement des sciences physiques". Science Resources for Teaching Physics (in French). 12 June 2003. Retrieved 19 October 2016..
  6. ^ Joseph, F. (1 December 1985). "Revue Pyrénéenne : Orages en Montagne". French National Library (in French). pp. 4–6. Retrieved 19 October 2016..
  7. ^ Thillet & Schueller 2009, p. 111
  8. ^ "Effet couronne sur les réseaux électriques aériens | Techniques de l'Ingénieur". www.techniques-ingenieur.fr. Retrieved 2016-10-19..
  9. ^ a b c d Chardon, Michel (1989). "Essai d'approche de la spécificité des milieux de la montagne alpine". Revue de géographie alpine. 77: 15–28. doi:10.3406/rga.1989.2727. Retrieved 2016-10-19..
  10. ^ "Petit manuel de météo de montagne". Le Guide Météo (in French). 2015-09-05. Retrieved 2016-10-19..
  11. ^ Champetier, JL. "QUE FAIRE EN CAS D'ORAGE". www.clubalpin-tarbes.org. Archived from the original on 2016-10-19. Retrieved 2016-10-19..
  12. ^ Thillet & Schueller 2009, p. 171
  13. ^ "Conditions montagne générales, alpinisme, cascades, ski". www.fondazionemontagnasicura.org. Retrieved 2016-11-01.
  14. ^ "KERAUNOS - Observatoire Français des Tornades et des Orages Violents - Prévision, suivi et étude des orages en France". www.keraunos.org. Retrieved 2016-11-01.
  15. ^ Bonington, Chris (2013-07-15). Les horizons lointains: Souvenirs d'une vie d'alpiniste (in French). Primento. ISBN 9782511006566. Retrieved 2016-10-22..
  16. ^ 1971 Arthaud, ISBN 208131343X, ISBN 9782081313439, 304 pages.
  17. ^ Walter Bonatti (1997). Montagnes d'une vie. Paris: Arthaud. p. chapitre XII « La grande tragédie du pilier central (1961). ISBN 2-7003-1144-2..
  18. ^ "Il y a 50 ans, la tragédie du Frêney". Le Dauphiné Libéré (in French). 17 July 2011. Retrieved 21 October 2016..
  19. ^ "[Association Pierre Kohlmann] Pierre Kohlmann". archive.is. Archived from the original on 2013-07-02. Retrieved 2016-10-21.((cite web)): CS1 maint: bot: original URL status unknown (link).
  20. ^ "The 1961 drama of the Central Pillar of Freney : Articles : SummitPost". www.summitpost.org. Retrieved 2023-09-30.

Bibliography

Further reading