Lawinenlagebericht

South Rockies

Mar 2 – 3, 2014Avalanche Canada
Auf der Karte ansehen
Archiviert · abgelaufen 13 years ago

Lawinengefahr

Tue
Wed
Hochgebirge
3 · Erheblich
Waldgrenze
3 · Erheblich
Unterhalb
3 · Erheblich

Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely
    Größe
    1–3
    Recent strong winds from the north resulted in reverse loading.  Winds are now from the SW and forming new wind slabs.  Expect wind slabs on all aspects in wind affected terrain.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    3–6
    Expect the buried persistent weak layer to continue to produce large and destructive avalanches. Many slopes are still primed for human triggering and remain a concern on all aspects and elevations.

Confidence

Fair

Weather Forecast

Unsettled conditions are expected for the forecast period with light flurries and periods of sun. A more organized system is expected for late-Wednesday or Thursday.Monday: Cloudy with sunny breaks, flurries 1-4cm, freezing level rising to around 1200m, ridgetop wind 40-60 SWTuesday: Cloudy with sunny breaks, flurries 3-6cm, freezing level around 1300m, ridgetop wind 30-50 SWWednesday: Cloudy with sunny breaks, flurries 3-6cm, freezing level around 1400m, ridgetop wind 20-40 SW

Avalanche Summary

We have not received any reports of new avalanches since the solar triggered activity a few days ago. However, recent snowpack tests imply that where the layer still exists, the potential for large, destructive avalanches still exists.

Snowpack Summary

The primary concern remains a persistent slab that sits on a stubborn persistent weak layer consisting of a crust, facets, and/or surface hoar. The layer continues to show a high degree of sensitivity to human triggers. Wide propagations and remote triggering remain a concern. In the thinner snowpack areas such as the Crowsnest and northern Elk Valley, the slab is typically 30-60cm thick. In thicker areas such as the Flathead and around Fernie, the slab typically varies in thickness from 70-150cm. Check out the South Rockies Blog for a video discussing the persistent weak layer and the current avalanche problem. Outflow winds from the N-NE created reverse-loaded wind slabs a few days ago. More recent strong SW winds have created new, touchy wind slabs on the opposite aspects.  Cornices remain a concern along ridge lines and threaten the slopes below. South facing slopes have formed a sun crust on the snow surface. New surface hoar formation up to 4mm and near-surface faceting are also being reported. A weakness at the base of the snowpack may still exist in isolated areas of the region but triggering has become unlikely.  New snowfall is currently burying this layer.

Abgedeckte Regionen