Wet Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1.5–2.5
The most recent freezing temperatures were recorded on the evening of March 16th. This destabilized the upper snowpack as meltwater moved through the snowpack. When this water pools at a crust or a weak layer, it can create a wet slab avalanche. With all of the crusts and weak layers that exist in our snowpack, we have the structure to potentially see large or very large wet slab avalanches. Consider this cooling trend a step in the right direction, but be patient as the upper snowpack may still need some time to refreeze. Today, get curious about the thickness of the refrozen surface and how wet the snow beneath this crust may be.
Wet slab avalanches are notoriously destructive and difficult to forecast. While the chance of triggering such an avalanche may be low, the consequence would likely be catastrophic. Be particularly cautious on sun-affected slopes or very steep slopes with rock outcroppings. If you see roller-balls, signs of recent avalanches, or find yourself sinking into wet, unconsolidated snow, move to lower-angle terrain until temperatures drop and the snowpack can stabilize.