Wet Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3
4" of liquid water (48-hour expected total) should be percolating through the Mt. Hood snowpack by the time surface temperatures cool early Wednesday morning. Snow levels will remain above the NWAC forecast area overnight before dropping rapidly early Wednesday. While the surface may gradually refreeze from the top down, plenty of water will continue to lubricate crusts in the snowpack. Prior to this storm cycle, the upper snowpack consists of mostly dry snow with a number of crusts interspersed within it. If water pools on any given layer, the saturated slab of snow above will create a large or even very large wet slab that could fail on slopes as shallow as 30 degrees. Wet slabs are very tricky to predict, so we may see no wet slabs or it could be more active than we expect. Evidence of recent large or very large avalanches is the first clue that things may be more dangerous. In the absence of direct evidence, you can also dig down a meter in the snowpack to see if there is free water in the snow. The best strategy when you have a low probability high consequence problem is often to steer around large avalanche paths, choosing smaller terrain features, ridges or forested terrain to maintain your margin of safety.
Shallow fresh snowfall may insulate the snow surface and help slow the refreeze. If you find wet or sticky snow that you can sink into up to your boot top, then steer around slopes steeper than 35 degrees to avoid a Wet Loose avalanche problem.
(1/12/2021) A very large natural wet avalanche in the Wellington slide path near Stevens Pass.