Avalanche Problems
There are nine different types of avalanche problems:
Storm slab
Wind slab
Wet slab avalanches
Persistent slab
Deep persistent slab
Loose dry avalanches
Loose wet avalanches
Glide avalanches
Cornice fall

Canadian classification for avalanche size
The Canadian classification for avalanche size is based upon the consequences of the avalanche. Half sizes are commonly used. United States classification for avalanche size
The size of avalanches are classified using two scales; size relative to destructive force or D-scale and size relative to the avalanche path or R-scale. Both size scales range from 1 to 5 with the D size scale half sizes can be used. Rutschblock Test
Slab avalanche hazard analysis can be done using the Rutschblock Test. A 2 m wide block of snow is isolated from the rest of the slope and progressively loaded. The result is a rating of slope stability on a seven step scale. (Rutsch means slide in German). Avalanches and climate change
Avalanche formation and frequency is highly affected by weather patterns and the local climate. Snowpack layers will form differently depending on whether snow is falling in very cold or very warm conditions, and very dry or very humid conditions. Thus, climate change may affect when, where, and how often avalanches occur, and may also change the type of avalanches that are occurring. Impacts on avalanche type and frequency
Overall, a rising seasonal snow line and a decrease in the number of days with snow cover are predicted.
In turn, socio-environmental changes can influence the occurrence of damaging avalanches: some studies linking changes in land-use/land-cover patterns and the evolution of snow avalanche damage in mid latitude mountains show the importance of the role played by vegetation cover, that is at the root of the increase of damage  when the protective forest is deforested (because of demographic growth, intensive grazing and industrial or legal causes), and at the root of the decrease of damage because of the transformation of a traditional land-management system based on overexploitation into a system based on land marginalization and reforestation, something that has happened mainly since the mid-20th century in mountain environments of developed countries

Mitigation
In many areas, regular avalanche tracks can be identified and precautions can be taken to minimize damage, such as the prevention of development in these areas. To mitigate the effect of avalanches the construction of artificial barriers can be very effective in reducing avalanche damage. There are several types: One kind of barrier (snow net) uses a net strung between poles that are anchored by guy wires in addition to their foundations. These barriers are similar to those used for rockslides. Another type of barrier is a rigid fence-like structure (snow fence) and may be constructed of steel, wood or pre-stressed concrete. They usually have gaps between the beams and are built perpendicular to the slope, with reinforcing beams on the downhill side. Rigid barriers are often considered unsightly, especially when many rows must be built.