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Fig. 10.7 The variation of number of days with snow depth within the Bâlea and Sinaia ski area
(on the left ) and the nivometric type of regime in the Bâlea and Sinaia ski areas
Fig. 10.8 Correlation between snow depth and snow avalanches, between 2005-2006 and
2006-2007
With regard to the same issue, the snow avalanche climatic potential, we have
analyzed the relation between snow depth and the snow avalanche frequency in
years with considerable snowfall (Fig. 10.8 ):
10.4 The Management of Snow Avalanche Risk
The Fagaras massif is characterized by high snow avalanche activity, especially in
the Bâlea ski area. Many snow avalanches are triggered by skiers as it is mentioned
in several works (Grímsd
ottir and McClung, 2006 ; Schweizer and Camponovo,
´
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