Lawinenlagebericht

South Rockies

Mar 30 – 31, 2014Avalanche Canada
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Archiviert · abgelaufen 13 years ago

Lawinengefahr

Tue
Wed
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
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Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Recent west winds have created wind slabs in the lee of terrain features.

  • Deep Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    3–6
    Deep persistent weak layers have a low probability of triggering. Possible triggers at this point include a large cornice fall, surface avalanche in motion or solar warming.

Confidence

Fair - Forecast snowfall amounts are uncertain on Monday

Weather Forecast

Monday: Mix of sun and cloud with possible intermittent flurries. Light west winds. Freezing level 1500m.Tuesday: Mainly sunny with some cloudy periods. Light westerly winds. Freezing level 1500m.Wednesday: Mix of sun and cloud. Freezing level 1800m. Light west winds.

Avalanche Summary

Recent observations indicate natural slab avalanche activity to size 2 in the alpine. This activity is isolated to the most recent storm snow. In addition loose moist snow avalanches to size 1.5 out of steep solar aspects in the alpine and at tree-line.

Snowpack Summary

See this great video from our South Rockies field team that does an awesome job of summarizing the current state of the mid to lower snowpack.Up to 30cm of recent new snow sits on top of a thick sun crust on solar aspects. 70-90 cm of settling storm snow from the past week rests on a graupel layer that can be found in much of the region. This makes for around 90 cm on top of the mid march crust at this point. This crust exists on all aspects below 2000m and on solar aspects in the high alpine. North of Sparwood and in the Crowsnest Pass area, the buried crust seems more specific to previously sun-exposed slopes. The deep facet/crust persistent weakness buried at the beginning of February (now down up to 150cm) seems unlikely to trigger in areas where the hard, supportive crust exists. No matter where you are in the region, this weakness should stay on your radar as any activity at this interface would be large and destructive. Possible triggers include a large cornice fall, a large input in a thin snowpack area or solar warming.

Abgedeckte Regionen