Wind Slabs
N
NE
E
SE
S
SW
W
NW
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–4
New wind slabs may have developed with recent snow and wind. Watch for these behind ridges and terrain breaks.
Lawinenlagebericht
Auf der Karte ansehenNorthwest Coastal
Apr 20 – 21, 2012Avalanche Canada
Archiviert · abgelaufen 14 years ago
Lawinengefahr
Sun
Mon
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
Lawinenprobleme
Loose Wet
NNEESESSWWNW- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible - Likely
- Größe
- 1–5
Loose wet avalanches are most likely during periods of warming from rainfall or sunshine. These can push you around, entrain mass and become surprisingly large.
Wet Slabs
NNEESESSWWNW- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–7
Warm temperatures or rain may continue to weaken the snowpack, leading to full-depth releases. Avoid traveling on or underneath any slopes which sport glide cracks. Large glide slabs have been releasing all week in specific terrain.
Confidence
Fair - Timing, track, or intensity of incoming weather is uncertain for the entire period
Weather Forecast
Saturday: Cloudy with scattered light precipitation possible. Light to moderate southerly winds. Freezing level around 1500 m.Sunday: Mainly dry and sunny. Freezing level around 1200 m, falling to near valley floor overnight. Light winds.Monday: Light, scattered precipitation. Freezing level rising to around 1000 m in the afternoon. Light winds.
Avalanche Summary
Reports of natural glide activity from the Skeena corridor continue. Cornice fall and ice fall triggered 1-1.5 m deep wet slabs in the Bear Pass area on Thursday.
Snowpack Summary
New wind slabs may have built on lee slopes. The snow surface below about 1000 m has not been re-freezing overnight, leading to weak soft snow. Large cornices and ice cliffs pose a threat from above.As we transition into spring, the surface layers have a great deal of influence on the snowpack. When there is a solid re-frozen surface crust, travel is fast and easy, and the snowpack is held together by the surface cap. Any deeper persistent weak layers are unlikely to fail until the surface cap breaks down from daytime heating. When there is no crust, surface layers and any deeper weak layers may fail, depending on the amount of heat and the triggering force that is applied. If it cools off and snows, new snow and wind slabs may not bond well to the hard spring crusts. For more information on Spring Conditions and ways to mitigate risk, please visit the new Forecasters' Blog Post.