Lawinenlagebericht

Lizard-Flathead

Dec 25 – 26, 2016Avalanche Canada
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Archiviert · abgelaufen 10 years ago

Lawinengefahr

Mon
Tue
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering

Kernpunkte

Strong winds will maintain dangerous avalanche conditions at higher elevations.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    1–2
    Expect fresh wind slabs to form as winds pick up and redistribute loose snow. If triggered, wind slabs could potentially step down to deeper weak layers.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

MONDAY: Isolated flurries with trace accumulations, 30-50 km/h southwest winds increasing throughout the day to 50-70 km/h in the evening, alpine temperatures -10C.TUESDAY: Flurries with accumulations up to 10 cm, 50 km/h southwest winds, alpine temperatures -5C.WEDNESDAY: Isolated flurries with trace accumulations, 50 km/h west winds, alpine temperatures -8C.

Avalanche Summary

The most recent low density snow produced several natural and explosive triggered size 1.5-2 avalanches over the weekend. Last week, explosive triggers released several larger avalanches (up to size 2.5) running on weak sugary facets between 40 and 100 cm deep.Wind slabs remain the primary concern for human-triggering, as they sit above weak sliding layers and will continue to build as winds pick up throughout Monday. Persistent slabs releasing on weak layers that formed in early December are also becoming a concern. The recent explosive results suggest these layers could potentially wake up with extra loading from new snow or wind, or possibly be triggered in shallow snowpack areas.

Snowpack Summary

Recent flurries delivered 15-30 cm of low density powder, which now sits above hard wind slabs and settled storm snow from last week. A variable interface that formed during the mid-December cold snap can be found 50-80 cm deep. This interface consists of hard wind packed snow in exposed terrain, weak faceted (sugary) snow, and surface hoar up to 20 mm in sheltered areas. This interface could evolve into a persistent slab problem once the storm snow settles into a slab. Deeper in the snowpack you may find another layer of surface hoar in sheltered areas or weak facets that were buried in early December. The thick crust from mid-November is near the bottom of the snowpack and reports suggest that the crust is currently well bonded to the surrounding snow.

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