Loose Wet
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–1.5
Heat from the sun and temperatures climbing above freezing lead to melting of the surface snow. As the proportion of liquid water to ice crystals increases the snow can no longer "cling" to the slope and a Wet loose avalanche occurrs. This type of avalanche is most prevalent on steep South slopes which receive the most heat from the sun. It is unlikely that this melting will extend much into the rain crust that exists in our upper snowpack, so any avalanches will be limited to the soft surface snow. On many aspects this snow is only a few inches deep, but on some wind loaded South slopes there is 10 inches to a foot of snow overlaying the crust. These are the slopes I would be careful on.