Avoid staying for a longer period in avalanche release and run out areas. For danger Level 3: Avoid avalanche release and run out areas.

Wet snow avalanches tend to release spontaneously.

Stability decreases when the snow surface gets wet and soft.

Timing is important.

Wet snow


  • The avalanche problem is related to wetting and weakening of the snowpack due to the presence of liquid water. Water infiltrates the snowpack due to melt or rain. 
  • The problem can occur due to rain, sun, warm temperatures or lack of refreezing of the snowpack at night.
  • Avalanches can vary in size from small to very large. Runout length can be very long with high water content.
  • Mainly natural release
  • Requires a snowpack with clear layering.
  • The probability for wet slab avalanches is at it's highest at first time wetting of a previous dry layered snowpack occurs.
  • Predicting the release of wet slab avalanches is difficult. It takes time for the water to penetrate into the snowpack and weaken the slab/weak layers enough for an avalanche to release.
  • If sun is the problem (typical spring conditions) - the danger increases during the day, most avalanches occur in afternoon when the temperature is higher.


Spatial distribution

  • When sun is the main cause, distribution of the problem is mostly depending on aspect and elevation.
  • All aspects are affected in the event of rain on snow.


Release characteristics

  • Warming leads to melting and weakening of pre-existing weak layers in the snowpack or ponding at layer interfaces.
  • If rain, there is also additional loading on weak layers.



Possible weak layers

  1. Water pooling in/above snow layers
  2. Buried weak layer of surface hoar
  3. Buried weak layer of faceted snow near surface
  4. Buried weak layer of faceted snow above a crust
  5. Buried weak layer of faceted snow beneath a crust
  6. Buried weak layer of faceted snow near the ground



  • Hours to days, depending on temperature, precipitation and radiation



Identification of the problem

  • Usually easy to recognize.
  • Wet and soft snow surface, onset of rain, snowballing, pin wheeling and small wet slabs or loose wet avalanches are often precursors of natural wet-snow slab avalanche activity.
  • Deep foot-penetration is another sign of increased wetting.


Wet slab avalanche. Photo: HåvardT/regObs