Wind Slabs
N
NE
E
SE
S
SW
W
NW
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible - Likely
- Größe
- 1–2
Winds slabs formed from recent W winds have now been buried by Saturdays snowfall and may be hard to detect.
Lawinenlagebericht
Auf der Karte ansehenWaterton Lakes
Feb 24 – 27, 2019Parks Canada
Archiviert · abgelaufen 8 years ago
Lawinengefahr
Mon
Tue
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
Kernpunkte
Recent snow has formed a slab overloading weak snow below treeline. This problem is compounded by the newly burnt forest, allowing wind to stiffen the snow all the way to valley bottom.
Lawinenprobleme
Deep Persistent Slabs
NNEESESSWWNW- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2.5
Recent snow has been enough to create a slab over deep instabilities below treeline where the snowpack is shallow and weak, and melt freeze crusts have been preserved. These were reactive to skier traffic on Mt. Bertha on Thursday.
Weather Forecast
Saturday: Mix of sun and cloud with light Northeast winds. Alpine High -15Sunday: Sunny with cloudy periods, light East winds. Temperature inversion, with an Alpine high of -19.Monday: Cloudy with isolated flurries, with up to 10cm on the front ranges, and less along the divide. Alpine high of -18
Snowpack Summary
The midpack remains strong in deep snowpack areas, but is acting as a slab above deep weak layers in shallower areas that is reactive skiers mainly at below treeline elevations where melt freeze crusts have been preserved. Continued snowfall on Saturday is burying windslabs formed by recent Westerly winds.
Avalanche Summary
We received a second hand report of skier triggered avalanches below treeline on Mt. Bertha on Thursday failing on facets above a crust deep in the snowpack, or basal facets. A natural size 2 slab was also observed below treeline in a steep and shallow snowpack feature in the Cameron Lake area that failed on similar weak layers earlier in the week.