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Debris flow hazards for mountain regions of Russia: regional features and key events

Author

Listed:
  • Veniamin Perov

    (M.V. Lomonosov Moscow State University)

  • Sergey Chernomorets

    (M.V. Lomonosov Moscow State University)

  • Olga Budarina

    (M.V. Lomonosov Moscow State University)

  • Elena Savernyuk

    (M.V. Lomonosov Moscow State University)

  • Tatiana Leontyeva

    (M.V. Lomonosov Moscow State University)

Abstract

The total area of debris flow territories of the Russian Federation accounts for about 10% of the area of the country. The highest debris flow activity areas located in Kamchatka-Kuril, North Caucasus and Baikal debris flow provinces. The largest debris flow events connected with volcano eruptions. Maximum volume of debris flow deposits per one event reached 500 × 106 m3 (lahar formed during the eruption of Bezymyanny volcano in Kamchatka in 1956). In the mountains of the Greater Caucasus, the maximum volume of transported debris material reached 3 × 106 m3; the largest debris flows here had glacial reasons. In the Baikal debris flow province, the highest debris flow activity located in the ridges of the Baikal rift zone (the East Sayan Mountains, the Khamar-Daban Ridge and the ridges of the Stanovoye Highland). Spatial features of debris flow processes within the territory of Russia are analyzed, and the map of Debris Flow Hazard in Russia is presented. We classified the debris flow hazard areas into 2 zones, 6 regions and 15 provinces. Warm and cold zones are distinguished. The warm zone covers mountainous areas within the southern part of Russia with temperate climate; rain-induced debris flows are predominant there. The cold zone includes mountainous areas with subarctic and arctic climate; they are characterized by a short warm period, the occurrence of permafrost, as well as the predominance of slush flows. Debris flow events are described for each province. We collected a list of remarkable debris flow events with some parameters of their magnitude and impact. Due to climate change, the characteristics of debris flows will change in the future. Availability of maps and information from previous events will allow to analyze the new cases of debris flows.

Suggested Citation

  • Veniamin Perov & Sergey Chernomorets & Olga Budarina & Elena Savernyuk & Tatiana Leontyeva, 2017. "Debris flow hazards for mountain regions of Russia: regional features and key events," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 88(1), pages 199-235, August.
  • Handle: RePEc:spr:nathaz:v:88:y:2017:i:1:d:10.1007_s11069-017-2841-3
    DOI: 10.1007/s11069-017-2841-3
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    References listed on IDEAS

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    1. Dieter Rickenmann, 1999. "Empirical Relationships for Debris Flows," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 19(1), pages 47-77, January.
    2. D. Petrakov & O. Tutubalina & A. Aleinikov & S. Chernomorets & S. Evans & V. Kidyaeva & I. Krylenko & S. Norin & M. Shakhmina & I. Seynova, 2012. "Monitoring of Bashkara Glacier lakes (Central Caucasus, Russia) and modelling of their potential outburst," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 61(3), pages 1293-1316, April.
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    Cited by:

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    2. Sven Fuchs & Alexandr Shnyparkov & Vincent Jomelli & Nikolay Kazakov & Sergey Sokratov, 2017. "Editorial to the special issue on natural hazards and risk research in Russia," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 88(1), pages 1-16, August.
    3. Liuqun Dong, 2023. "Energy consumption analysis of the granular run-out process: effect of particle shape and slope angle," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 117(2), pages 1673-1687, June.

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