Lawinenlagebericht

South Columbia

Dec 5 – 6, 2013Avalanche Canada
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Archiviert · abgelaufen 13 years ago

Lawinengefahr

Sat
Sun
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering

Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Strong NE winds have redistributed loose surface snow into reactive wind slabs on southwest facing terrain. This is an atypical loading pattern which has the potential to catch skiers/riders by surprise.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–4
    This persistent slab will be tricky to manage as it overlies a variety of weak surfaces. A conservative and investigative approach is required for safe mountain travel.

Confidence

Fair - Due to the number of field observations

Weather Forecast

A strong Arctic air mass will continue to dominate conditions in the southern interior. Friday: Mostly sunny, light NE alpine winds, alpine temperatures -20 to -25CSaturday: Mostly sunny, light-moderate NE alpine winds, alpine temperatures as low as -30CSunday: Increased cloud cover, moderate alpine winds, alpine temperatures as low as -25C, very light snowfall possible

Avalanche Summary

Fewer natural avalanches are occurring in the region but a few natural slab avalanches up to size 2 have been reported. These are both wind slabs and previous storm snow sliding on the late-November crust/surface hoar interface.

Snowpack Summary

Snowpack depths are typically 100-140 cm at treeline elevation. The previous storm snow (~30-60cm) overlies the late-November interface which typically consists of sun crusts on steep south facing slopes and surface hoar in sheltered areas. These weak layers are expected to be persistent and will continue to create avalanche problems in areas with enough overlying snow. The current cold temperatures will contribute to the persistence of this weak layer. Strong NE winds after the storm have caused reverse loading and wind slab formation on SE through W aspects in wind exposed areas. There are two layers of concern within the mid/lower snowpack but these have recently become inactive: the early November surface hoar is roughly 60cm above the ground and the October rain crust is at the base of the snowpack. While these layers have recently become inactive, residual risk of large, destructive avalanches exists, especially in areas with a thinner snowpack. The October crust can be found in the alpine on north aspects and the early November surface hoar appears to be isolated and drainage specific.

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