Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Rapid loading through Monday produced numerous natural avalanches.
We have seen a significant avalanche cycle in Waterton over the last couple days, new snow has overburdened buried weak layers and produced large avalanches. Use cautious terrain management over the next few days as avalanches will continue to be human triggerable.
Rapid loading through Monday produced numerous natural avalanches.
New wind load is causing the January 31st drought layer to fail in many places
Pay special attention to steep slopes when the sun is out.
Widespread natural cycle over the last few days with windslab, wet loose and persistent slab avalanches to size 3
The notable size 3 avalanche was on Bertha Mountain above the Waterton Townsite and deposited debris within 100m of town.
~30 cm of storm snow has fallen over the last few days, this snow arrived with winds up to 70km/h. This has formed windslabs in the alpine/treeline. It rained below 1800 m and saturated the snowpack.
The January drought layer is 30 - 60 cm down. This layer includes facetted snow on northerly aspects or a melt freeze crust below treeline and on steep solar slopes into the alpine. Generally, the snowpack is weak and facetted.
Snowpack depths at treeline range from 100 - 160 cm.
Warm temps and strong winds continue for the next few days. See table for details.
Check out the Mountain Weather Forecast for the most up to date information.