Lawinenlagebericht

South Columbia

Dec 21, 2017Avalanche Canada
Auf der Karte ansehen
Archiviert · abgelaufen 9 years ago

Lawinengefahr

Fri
Sat
Hochgebirge
3 · Erheblich
Waldgrenze
3 · Erheblich
Unterhalb
3 · Erheblich

Kernpunkte

Choose conservative terrain in the coming days as recent storm slab continues to settle and consolidate. 

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Recent west and northwest winds switching to north and northeast have formed windslabs in the lee of terrain features on a variety of aspects.
  • Storm Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    1–3
    As the recent new snow continues to settle and consolidate over the next few days, expect it to become more reactive to human triggering where it may be sitting on layer of weak feathery surface hoar.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

THURSDAY: Cloudy with flurries, accumulation 5cm / wind light to moderate northwest / alpine temperature -9FRIDAY: Mix of sun and cloud / wind light north / alpine temperature -14 SATURDAY: Mainly sunny / wind moderate northwest / alpine temperature -12

Avalanche Summary

Reports from the past few days include explosives controlled and natural storm snow avalanches to size 2.5 in the alpine and tree line. There have also been a several reports of skier accidental and skier remote (triggered from a distance) avalanches to size 1.5 at and below tree line. As the new snow settles and consolidates in the coming days expect to see in human triggered avalanche activity continue even as the stormy period ends.

Snowpack Summary

The 40-70cm of new snow accumulating since last Friday now sits on a wide variety of old surfaces including large surface hoar (weak, feather-like crystals), hard crusts formed by sun or wind, and sugary facets. As the snow load builds and slab properties develop, it will be important to monitor how the new snow is bonding to the old surfaces. Most concerning would be areas that have seen previous surface hoar development, such as sheltered areas at and below tree line and sheltered northerly aspects in the alpine. Additionally, any steep solar aspects where the surface hoar may be sitting on sun crust should be considered areas where this weak layer may be very likely to trigger.A crust which was formed by rain in late November is a major feature in the snowpack and is down approximately 70-100cm at tree line elevations. Snowpack tests suggest the snow above is currently bonding well to it. Snowpack depth decreases rapidly below tree line. Look out for early season hazards such as rocks, stumps, and open creeks.

Abgedeckte Regionen