Zobrazeno 1 - 5
of 5
pro vyhledávání: '"T. G. Glazovskaya"'
Publikováno v:
Лëд и снег, Vol 59, Iss 2, Pp 245-257 (2019)
The legislation of the Russian Federation establishes the need to take into account hazardous natural processes and their parameters in territorial planning, as well as presentation of them in the relevant documentation in the form of maps. In a numb
Externí odkaz:
https://doaj.org/article/813b13dab8f54d288137be62cb2aa3e2
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 16, Pp 2227-2234 (2016)
Avalanches pose a significant problem in most mountain regions of Russia. The constant growth of economic activity, and therefore the increased avalanche hazard, in the North Caucasus region lead to demand for the development of large-scale avalan
Externí odkaz:
https://doaj.org/article/5fad717c11004fbaa93c0e2b266a6a06
Avalanche pose a significant problem in most mountain regions of Russia. The constant growth of economic activity in highlands and the increased avalanche hazard lead to the demand to develop the methods of large-scale avalanche hazard assessment. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c8ec1fd256c20b6952c56f13ad04451
https://doi.org/10.5194/nhess-2016-68
https://doi.org/10.5194/nhess-2016-68
Autor:
T. G. Glazovskaya, Ksenia Sergeeva, Alexander Shnyparkov, Yuri Seliverstov, Alexei Martynov, Yana Vilchek
Publikováno v:
Annals of Glaciology. 49:205-209
The term ‘risk’ can be defined as the probability of unfavourable consequences or negative effects. Risk can be expressed by means of various indices, such as collective or social risk (possible number of dead), individual risk (probability of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6bb667facb3d509ca84e01d502403ab
https://doi.org/10.3189/172756408787814672
https://doi.org/10.3189/172756408787814672
Autor:
T. G. Glazovskaya
Publikováno v:
Annals of Glaciology. 26:337-342
Snow avalanches occur in the mountains of all continents and climatic zones. The lower boundary of avalanche distribution rises from sea level in polar and temperate zones to 6000 m in the tropics. Four altitudinal belts of avalanching are distinguis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c0e1cae82960062783f7d6d12be97e2
https://doi.org/10.3189/1998aog26-1-337-342
https://doi.org/10.3189/1998aog26-1-337-342