Assessment of the economic risk for the ski resorts of changes in snow cover duration

Winter tourism that is intensively developed in the Russian Federation in recent years strongly depends on the snow availability and properties in the region. Climate changes exert significant influence on the functioning of mountain ski resorts, especially if they are located in areas with relative...

Full description

Bibliographic Details
Published in:Ice and Snow
Main Authors: S. Sokratov A., Yu. Seliverstov G., A. Shnyparkov L., С. Сократов А., Ю. Селиверстов Г., А. Шныпарков Л.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2015
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/60
https://doi.org/10.15356/2076-6734-2014-3-100-106
id ftjias:oai:oai.ice.elpub.ru:article/60
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Risk;ski resorts;snow cover
Горнолыжные курорты;риск;снежный покров
spellingShingle Risk;ski resorts;snow cover
Горнолыжные курорты;риск;снежный покров
S. Sokratov A.
Yu. Seliverstov G.
A. Shnyparkov L.
С. Сократов А.
Ю. Селиверстов Г.
А. Шныпарков Л.
Assessment of the economic risk for the ski resorts of changes in snow cover duration
topic_facet Risk;ski resorts;snow cover
Горнолыжные курорты;риск;снежный покров
description Winter tourism that is intensively developed in the Russian Federation in recent years strongly depends on the snow availability and properties in the region. Climate changes exert significant influence on the functioning of mountain ski resorts, especially if they are located in areas with relatively high air temperatures in winter season. At the present time, a snowy cluster of mountain ski resorts is intensively progressing in vicinity of Krasnaya Polyana. This region in the West Caucasus (Russia) is characterized by relatively warm climate conditions. The snow cover thickness (of 1% insurance) in area of the Aibga mountain range may reach 8.1 m. But the snow cover thickness is not the only characteristic of the mountain skiing attractiveness. According to the Swiss standards a mountain ski resort can be considered reliable if during seven seasons of ten ones the snow cover with minimal thickness of 30–50 cm exists for a time not shorter than 100 days during a period from 1st December till 15th April.According to the forecast, during future decades the calculated amount of solid precipitation should reduce by 25–30% in mountain regions on the south macro-slope of the Great Caucasus. As the calculations show, by 2041–2050 the maximal decade thickness of snow cover will decrease by 29–35% while a number of days with snow – by 35–40%. If this is the case, artificial snow will be needed in addition to the natural one. But, under warm climate conditions using of plants for artificial snow production will require a certain perfecting of the nowadays technologies, and very likely, with use of chemicals. That is why a shadowing of existing mountain ski routes by means of the tree planting along them could be ecologically more promising. As for the mountain ski resorts of the West Caucasus, we should mention a possible weakening of the avalanche activity as a potential positive effect of the climate warming predicted by models. На примере района Красной Поляны рассматривается зависимость надёжности функционирования ...
format Article in Journal/Newspaper
author S. Sokratov A.
Yu. Seliverstov G.
A. Shnyparkov L.
С. Сократов А.
Ю. Селиверстов Г.
А. Шныпарков Л.
author_facet S. Sokratov A.
Yu. Seliverstov G.
A. Shnyparkov L.
С. Сократов А.
Ю. Селиверстов Г.
А. Шныпарков Л.
author_sort S. Sokratov A.
title Assessment of the economic risk for the ski resorts of changes in snow cover duration
title_short Assessment of the economic risk for the ski resorts of changes in snow cover duration
title_full Assessment of the economic risk for the ski resorts of changes in snow cover duration
title_fullStr Assessment of the economic risk for the ski resorts of changes in snow cover duration
title_full_unstemmed Assessment of the economic risk for the ski resorts of changes in snow cover duration
title_sort assessment of the economic risk for the ski resorts of changes in snow cover duration
publisher IGRAS
publishDate 2015
url https://ice-snow.igras.ru/jour/article/view/60
https://doi.org/10.15356/2076-6734-2014-3-100-106
genre Annals of Glaciology
Arctic
The Cryosphere
genre_facet Annals of Glaciology
Arctic
The Cryosphere
op_source Ice and Snow; Том 54, № 3 (2014); 100-106
Лёд и Снег; Том 54, № 3 (2014); 100-106
2412-3765
2076-6734
10.15356/2076-6734-2014-3
op_relation https://ice-snow.igras.ru/jour/article/view/60/33
Anisimov O.A. Present-day and future changes of permafrost: synthesis of observations and modeling. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2008, 1 (78): 7–16. [In Russian].
Atlas snezhno-ledovykh resursev mira. World Atlas of Snow and Ice Resources. V. 1. Ed. V.M. Kotlyakov. Moscow: Russian Academy of Sciences, 1997: 392 p.
Borzenkova A.B., Shmakin A.B. Changes of snow depth and daily intensity of snowfalls influenced to the expenses of highways cleaning in the Russian cities. Led i Sneg. Ice and Snow. 2012, 2 (118): 59–70. [In Russian].
Glyatsiologicheskiy slovar’. Glaciological Glossary. Ed. V.M. Kotlyakov. Leningrad: Hydrometeoizdat, 1984: 528 p. [In Russian].
Oleynikov A.B. Snow resources of the Krasnaya Polyana region (West Caucasus). Led i Sneg. Ice and Snow. 2013, 4 (124): 83–94. [In Russian].
Mal’neva I.V., Kononova N.K. Activity of mudflows at the territory of Russia and surrounding countries in XXI century. Georisk. 2012, 4: 48–54. [In Russian].
Rayonirovanie territorii Rossiyskoy Federatsii po vesu snezhnogo pokrova. Regionalization of the territory of Russian Federation according to the weight of snow. Technical document. Moscow: Ministry of the Regional Development of Russian Federation, 2011: 12 p. [In Russian].
Richter G.D. Use of snow in the national economy. Voprosy izucheniya snega i ispolzovaniya ego v narodnom khozyaystve. Problems of snow studies and use of snow in the national economy. Moscow: USSR Academy of Sciences, 1955: 5–22. [In Russian].
Seliverstov Yu.G., Glazovskaya T.G., Volodicheva N.A., Oleynikov A.D., Klimenko E.S., Samokhina E.A., Shnyparkov A.L. Assessment of avalanche danger in the mountain climatic resort “Alpica-Service”. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2012, 1: 31–38. [In Russian].
Formozov A.N. Snezhnyi pokrov kak factor sredy, ego znachenie v zhizni mlekopitayushchikh i ptits SSSR. Snow cover as a factor of the environment, its role in the life of mammalian and birds. Moscow State University, 1990: 268 p. [In Russian].
Shkol’nik I.M., Meleshko V.P., Kattsov V.M. Possible changes of climate at the European part of Russia and surrounding territories to the end of XXI century: calculation with the regional model of GGO. [In Russian]. Meteorologiya i gidrologiya. Meteorology and Hydrology. 2006, 3: 5–16.
Shul’gin A.M. Snezhnaya melioratsiya i klimat pochvy. Snow melioration and soil climate. Leningrad: Hydrometeoizdat, 1986: 72 p. [In Russian].
Ager B. Studier över klimatet i Norrland, Dalarna och Värmland: Studies of the Climate in North and Central Sweden (Studia Forestalia Suecica, Nr. 19). Stockholm: Skogshögskolan, 1964: 105 s.
Breiling M., Charamza P. The impact of global warming on winter tourism and skiing: a regionalised model for Austrian snow conditions. Regional Environmental Change. 1999, 1 (1): 4–14. doi:10.1007/s101130050003.
Breiling M., Charamza P., Skage O.R. Klimasensibilität österreichischer Bezirke mit besonderer Berücksichtigung des Wintertourismus (Institutionen för landskapsplanering Alnarp: Rapport 97:1). Alnarp: Sveriges Lantbruksuniversitet, 1997: 102 s.
Callaghan T.V., Johansson M., Brown R.D., Groisman P.Ya, Labba N., Radionov V., Barry R.G., Blangy S., Bradley R.S., Bulygina O.N., Christensen T.R., Colman J., Essery R.L.H., Forbes B., Forchhammer M.C., Frolov D.M., Golubev V.N., Grenfell T.C., Honrath R.E., Juday G.P., Melloh R., Meshcherskaya A.V., Petrushina M.N., Phoenix G.K., Pomeroy J., Rautio A., Razuvaev V.N., Robinson D.A., Romanov P., Schmidt N.M., Serreze M.C., Shevchenko V., Shiklomanov A.I., Shindell D., Shmakin A.B., Sköld P., Sokratov S.A., Sturm M., Warren S., Woo M.-k., Wood E.F., Yang D. Changing snow cover and its impacts. Snow, Water, Ice and Permafrost in the Arctic (SWIPA): Climate Change and the Cryosphere. Oslo: Arctic Monitoring and Assessment Programme (AMAP), 2011: 4-1 – 4-58.
Elsasser H., Bürki R. Climate change as a threat to tourism in the Alps. Climate Research. 2002: 20 (3): 253–257. doi:10.3354/cr020253.
Glazovskaya T.G. Global distribution of snow avalanches and changing activity in the Northern Hemisphere due to climate change. Annals of Glaciology. 1998, 26: 337–342.
Gonseth C. Impact of snow variability on the Swiss winter tourism sector: implications in an era of climate change. Climatic Change. 2013, 119 (2): 307–320. doi:10.1007/s10584-013-0718-3.
Hatanaka K.-i., Breiling M., Sato Y., Charamza P. Significance of winter tourism in hilly and mountainous areas of Japan. SEPPYO: Journ. of the Japanese Society of Snow and Ice. 2006, 68 (1): 15–29.
de Jong C., Masure P., Barth T. Challenges of alpine catchment management under changing climatic and anthropogenic pressures. Proc. of the iEMSs Fourth Biennial Meeting: Intern. Congress on Environmental Modelling and Software iEMSs 2008; Integrating Sciences and Information Technology for Environmental Assessment and Decision Making. V. 1. Eds. M. Sànchez-Marrè, J. Béjar, J. Comas, A. Rizzoli, G. Guariso. Barcelona: International Environmental Modelling and Software Society, 2008: 694–702.
Keller F., Frauenfelder R., Gardaz J., Hoelzle M., Kneisel C., Lugon R., Phillips M., Reynard E., Wenker L. Permafrost map of Switzerland. PERMAFROST – 7th Intern. Conf., June 23–27, 1998, Yellowknife, Canada (Collection Nordicana, № 57). Eds. A.G. Lewkowicz, M. Allard. Québec: Centre d'études nordiques, Université Laval, 1998: 557–562.
Marty C. Regime shift of snow days in Switzerland. Geophys. Research Letters. 2008, 35 (12): L12501. doi:10.1029/2008GL033998.
Mihashi H., Takahashi T. Japanese recommendation 1993 for snow loads on buildings. Snow Engineering: Recent Advances (Proc. of the Third Intern. Conf. on Snow Engineering, Sendai, Japan, 26–31 May 1996). Eds. M. Izumi, Ts. Nakamura, R.L. Sack. Rotterdam, Brookfield: A.A. Balkema, 1997: 215–222.
Morrison C., Pickering C.M. Perceptions of climate change impacts, adaptation and limits to adaption in the Australian Alps: the ski-tourism industry and key stakeholders. Journ. of Sustainable Tourism. 2013,21 (2): 173–191. doi:10.1080/09669582.2012.681789.
Sack R.L. Perspectives on the science, engineering and effects of snow. Snow Engineering: Recent Advances (Proc. of the Third Intern. Conf. on Snow Engineering, Sendai, Japan, 26–31 May 1996). Eds. M. Izumi, Ts. Nakamura, R.L. Sack. Rotterdam, Brookfield: A.A. Balkema, 1997: 3–10.
Scott D., Dawson J., Jones B. Climate change vulnerability of the US Northeast winter recreation- tourism sector. Mitigation and Adaptation Strategies for a Global Change. 2008, 13 (5–6): 577–596. doi:10.1007/s11027-007-9136-z.
Spreitzhofer G., Sperka S., Steinacker R. MetGIS™: combination of Meteorological and Geographic Information Systems to produce high resolution mountain weather forecasts. Meteorological Applications. 2013, 20 (3): 371–378. doi:10.1002/met.1299.
Uhlmann B., Goyette S., Beniston M. Sensitivity analysis of snow patterns in Swiss ski resorts to shifts in temperature, precipitation and humidity under conditions of climate change. Intern. Journ. of Climatology. 2009, 29 (8): 1048–1055. doi:10.1002/joc.1786.
Wolfsegger Ch., Gössling S., Scott D. Climate change risk appraisal in the Austrian ski industry. Tourism Review International. 2008, 12 (1): 13–23. doi:10.3727/154427208785899948.
Технический отчёт по инженерно-гидрометеорологическим изысканиям на объекте: «Горно-туристический центр открытого акционерного общества «Газпром», в том числе канатные дороги и горнолыжные спуски, объекты инженерной и транспортной инфраструктуры (проектные и изыскательские работы, строительство). Девятый этап строительства. ООО «ГЕО-ИНЖИНИРИНГ», 2010. 101 с.
https://ice-snow.igras.ru/jour/article/view/60
doi:10.15356/2076-6734-2014-3-100-106
op_rights Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access).
op_rightsnorm CC-BY
op_doi https://doi.org/10.15356/2076-6734-2014-3-100-106
https://doi.org/10.15356/2076-6734-2014-3
https://doi.org/10.1007/s101130050003
https://doi.org/10.3354/cr020253
https://doi.org/10.1007/s10584-013-0718-3
https://doi.org/10.1029/2008GL033998
h
container_title Ice and Snow
container_volume 127
container_issue 3
container_start_page 100
_version_ 1766003875463036928
spelling ftjias:oai:oai.ice.elpub.ru:article/60 2023-05-15T13:29:51+02:00 Assessment of the economic risk for the ski resorts of changes in snow cover duration Оценка экономического риска для горнолыжных курортов, связанного с изменением продолжительности залегания снежного покрова S. Sokratov A. Yu. Seliverstov G. A. Shnyparkov L. С. Сократов А. Ю. Селиверстов Г. А. Шныпарков Л. 2015-03-27 application/pdf https://ice-snow.igras.ru/jour/article/view/60 https://doi.org/10.15356/2076-6734-2014-3-100-106 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/60/33 Anisimov O.A. Present-day and future changes of permafrost: synthesis of observations and modeling. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2008, 1 (78): 7–16. [In Russian]. Atlas snezhno-ledovykh resursev mira. World Atlas of Snow and Ice Resources. V. 1. Ed. V.M. Kotlyakov. Moscow: Russian Academy of Sciences, 1997: 392 p. Borzenkova A.B., Shmakin A.B. Changes of snow depth and daily intensity of snowfalls influenced to the expenses of highways cleaning in the Russian cities. Led i Sneg. Ice and Snow. 2012, 2 (118): 59–70. [In Russian]. Glyatsiologicheskiy slovar’. Glaciological Glossary. Ed. V.M. Kotlyakov. Leningrad: Hydrometeoizdat, 1984: 528 p. [In Russian]. Oleynikov A.B. Snow resources of the Krasnaya Polyana region (West Caucasus). Led i Sneg. Ice and Snow. 2013, 4 (124): 83–94. [In Russian]. Mal’neva I.V., Kononova N.K. Activity of mudflows at the territory of Russia and surrounding countries in XXI century. Georisk. 2012, 4: 48–54. [In Russian]. Rayonirovanie territorii Rossiyskoy Federatsii po vesu snezhnogo pokrova. Regionalization of the territory of Russian Federation according to the weight of snow. Technical document. Moscow: Ministry of the Regional Development of Russian Federation, 2011: 12 p. [In Russian]. Richter G.D. Use of snow in the national economy. Voprosy izucheniya snega i ispolzovaniya ego v narodnom khozyaystve. Problems of snow studies and use of snow in the national economy. Moscow: USSR Academy of Sciences, 1955: 5–22. [In Russian]. Seliverstov Yu.G., Glazovskaya T.G., Volodicheva N.A., Oleynikov A.D., Klimenko E.S., Samokhina E.A., Shnyparkov A.L. Assessment of avalanche danger in the mountain climatic resort “Alpica-Service”. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2012, 1: 31–38. [In Russian]. Formozov A.N. Snezhnyi pokrov kak factor sredy, ego znachenie v zhizni mlekopitayushchikh i ptits SSSR. Snow cover as a factor of the environment, its role in the life of mammalian and birds. Moscow State University, 1990: 268 p. [In Russian]. Shkol’nik I.M., Meleshko V.P., Kattsov V.M. Possible changes of climate at the European part of Russia and surrounding territories to the end of XXI century: calculation with the regional model of GGO. [In Russian]. Meteorologiya i gidrologiya. Meteorology and Hydrology. 2006, 3: 5–16. Shul’gin A.M. Snezhnaya melioratsiya i klimat pochvy. Snow melioration and soil climate. Leningrad: Hydrometeoizdat, 1986: 72 p. [In Russian]. Ager B. Studier över klimatet i Norrland, Dalarna och Värmland: Studies of the Climate in North and Central Sweden (Studia Forestalia Suecica, Nr. 19). Stockholm: Skogshögskolan, 1964: 105 s. Breiling M., Charamza P. The impact of global warming on winter tourism and skiing: a regionalised model for Austrian snow conditions. Regional Environmental Change. 1999, 1 (1): 4–14. doi:10.1007/s101130050003. Breiling M., Charamza P., Skage O.R. Klimasensibilität österreichischer Bezirke mit besonderer Berücksichtigung des Wintertourismus (Institutionen för landskapsplanering Alnarp: Rapport 97:1). Alnarp: Sveriges Lantbruksuniversitet, 1997: 102 s. Callaghan T.V., Johansson M., Brown R.D., Groisman P.Ya, Labba N., Radionov V., Barry R.G., Blangy S., Bradley R.S., Bulygina O.N., Christensen T.R., Colman J., Essery R.L.H., Forbes B., Forchhammer M.C., Frolov D.M., Golubev V.N., Grenfell T.C., Honrath R.E., Juday G.P., Melloh R., Meshcherskaya A.V., Petrushina M.N., Phoenix G.K., Pomeroy J., Rautio A., Razuvaev V.N., Robinson D.A., Romanov P., Schmidt N.M., Serreze M.C., Shevchenko V., Shiklomanov A.I., Shindell D., Shmakin A.B., Sköld P., Sokratov S.A., Sturm M., Warren S., Woo M.-k., Wood E.F., Yang D. Changing snow cover and its impacts. Snow, Water, Ice and Permafrost in the Arctic (SWIPA): Climate Change and the Cryosphere. Oslo: Arctic Monitoring and Assessment Programme (AMAP), 2011: 4-1 – 4-58. Elsasser H., Bürki R. Climate change as a threat to tourism in the Alps. Climate Research. 2002: 20 (3): 253–257. doi:10.3354/cr020253. Glazovskaya T.G. Global distribution of snow avalanches and changing activity in the Northern Hemisphere due to climate change. Annals of Glaciology. 1998, 26: 337–342. Gonseth C. Impact of snow variability on the Swiss winter tourism sector: implications in an era of climate change. Climatic Change. 2013, 119 (2): 307–320. doi:10.1007/s10584-013-0718-3. Hatanaka K.-i., Breiling M., Sato Y., Charamza P. Significance of winter tourism in hilly and mountainous areas of Japan. SEPPYO: Journ. of the Japanese Society of Snow and Ice. 2006, 68 (1): 15–29. de Jong C., Masure P., Barth T. Challenges of alpine catchment management under changing climatic and anthropogenic pressures. Proc. of the iEMSs Fourth Biennial Meeting: Intern. Congress on Environmental Modelling and Software iEMSs 2008; Integrating Sciences and Information Technology for Environmental Assessment and Decision Making. V. 1. Eds. M. Sànchez-Marrè, J. Béjar, J. Comas, A. Rizzoli, G. Guariso. Barcelona: International Environmental Modelling and Software Society, 2008: 694–702. Keller F., Frauenfelder R., Gardaz J., Hoelzle M., Kneisel C., Lugon R., Phillips M., Reynard E., Wenker L. Permafrost map of Switzerland. PERMAFROST – 7th Intern. Conf., June 23–27, 1998, Yellowknife, Canada (Collection Nordicana, № 57). Eds. A.G. Lewkowicz, M. Allard. Québec: Centre d'études nordiques, Université Laval, 1998: 557–562. Marty C. Regime shift of snow days in Switzerland. Geophys. Research Letters. 2008, 35 (12): L12501. doi:10.1029/2008GL033998. Mihashi H., Takahashi T. Japanese recommendation 1993 for snow loads on buildings. Snow Engineering: Recent Advances (Proc. of the Third Intern. Conf. on Snow Engineering, Sendai, Japan, 26–31 May 1996). Eds. M. Izumi, Ts. Nakamura, R.L. Sack. Rotterdam, Brookfield: A.A. Balkema, 1997: 215–222. Morrison C., Pickering C.M. Perceptions of climate change impacts, adaptation and limits to adaption in the Australian Alps: the ski-tourism industry and key stakeholders. Journ. of Sustainable Tourism. 2013,21 (2): 173–191. doi:10.1080/09669582.2012.681789. Sack R.L. Perspectives on the science, engineering and effects of snow. Snow Engineering: Recent Advances (Proc. of the Third Intern. Conf. on Snow Engineering, Sendai, Japan, 26–31 May 1996). Eds. M. Izumi, Ts. Nakamura, R.L. Sack. Rotterdam, Brookfield: A.A. Balkema, 1997: 3–10. Scott D., Dawson J., Jones B. Climate change vulnerability of the US Northeast winter recreation- tourism sector. Mitigation and Adaptation Strategies for a Global Change. 2008, 13 (5–6): 577–596. doi:10.1007/s11027-007-9136-z. Spreitzhofer G., Sperka S., Steinacker R. MetGIS™: combination of Meteorological and Geographic Information Systems to produce high resolution mountain weather forecasts. Meteorological Applications. 2013, 20 (3): 371–378. doi:10.1002/met.1299. Uhlmann B., Goyette S., Beniston M. Sensitivity analysis of snow patterns in Swiss ski resorts to shifts in temperature, precipitation and humidity under conditions of climate change. Intern. Journ. of Climatology. 2009, 29 (8): 1048–1055. doi:10.1002/joc.1786. Wolfsegger Ch., Gössling S., Scott D. Climate change risk appraisal in the Austrian ski industry. Tourism Review International. 2008, 12 (1): 13–23. doi:10.3727/154427208785899948. Технический отчёт по инженерно-гидрометеорологическим изысканиям на объекте: «Горно-туристический центр открытого акционерного общества «Газпром», в том числе канатные дороги и горнолыжные спуски, объекты инженерной и транспортной инфраструктуры (проектные и изыскательские работы, строительство). Девятый этап строительства. ООО «ГЕО-ИНЖИНИРИНГ», 2010. 101 с. https://ice-snow.igras.ru/jour/article/view/60 doi:10.15356/2076-6734-2014-3-100-106 Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). CC-BY Ice and Snow; Том 54, № 3 (2014); 100-106 Лёд и Снег; Том 54, № 3 (2014); 100-106 2412-3765 2076-6734 10.15356/2076-6734-2014-3 Risk;ski resorts;snow cover Горнолыжные курорты;риск;снежный покров info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-3-100-106 https://doi.org/10.15356/2076-6734-2014-3 https://doi.org/10.1007/s101130050003 https://doi.org/10.3354/cr020253 https://doi.org/10.1007/s10584-013-0718-3 https://doi.org/10.1029/2008GL033998 h 2022-12-20T13:30:01Z Winter tourism that is intensively developed in the Russian Federation in recent years strongly depends on the snow availability and properties in the region. Climate changes exert significant influence on the functioning of mountain ski resorts, especially if they are located in areas with relatively high air temperatures in winter season. At the present time, a snowy cluster of mountain ski resorts is intensively progressing in vicinity of Krasnaya Polyana. This region in the West Caucasus (Russia) is characterized by relatively warm climate conditions. The snow cover thickness (of 1% insurance) in area of the Aibga mountain range may reach 8.1 m. But the snow cover thickness is not the only characteristic of the mountain skiing attractiveness. According to the Swiss standards a mountain ski resort can be considered reliable if during seven seasons of ten ones the snow cover with minimal thickness of 30–50 cm exists for a time not shorter than 100 days during a period from 1st December till 15th April.According to the forecast, during future decades the calculated amount of solid precipitation should reduce by 25–30% in mountain regions on the south macro-slope of the Great Caucasus. As the calculations show, by 2041–2050 the maximal decade thickness of snow cover will decrease by 29–35% while a number of days with snow – by 35–40%. If this is the case, artificial snow will be needed in addition to the natural one. But, under warm climate conditions using of plants for artificial snow production will require a certain perfecting of the nowadays technologies, and very likely, with use of chemicals. That is why a shadowing of existing mountain ski routes by means of the tree planting along them could be ecologically more promising. As for the mountain ski resorts of the West Caucasus, we should mention a possible weakening of the avalanche activity as a potential positive effect of the climate warming predicted by models. На примере района Красной Поляны рассматривается зависимость надёжности функционирования ... Article in Journal/Newspaper Annals of Glaciology Arctic The Cryosphere Ice and Snow (E-Journal) Ice and Snow 127 3 100