Lawinenlagebericht

South Rockies

Jan 18 – 19, 2013Avalanche Canada
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Archiviert · abgelaufen 14 years ago

Lawinengefahr

Sun
Mon
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering
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Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–4
    Strong to extreme winds out of the W/NW have left hard slabs, soft slabs, sastrugi and potentially unstable cornices in their wake. Watch for wind slabs behind midslope features like ridges and ribs. Be alert for wind slabs in unusual locations.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    1–5
    While unlikely, slopes that didn't slide in the last avalanche cycle may still be of concern this weekend. Triggering is most likely in areas that go from thick to thin in steep unsupported terrain.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Saturday: Inverted temperatures.  Below freezing at valley bottom, slightly above freezing in the alpine.  Strong ridgetop winds out of the NW.  No precip expected.Sunday: Freezing level starts at valley bottom, rises to 1000m during the day.  Winds start strong out of the NW, backing down to moderate by dinner time.  Trace of snow in the morning.Monday: Below freezing at valley bottom, slightly above freezing in the alpine. Ridgetop winds mod/strong west.  No precip expected.

Avalanche Summary

A few loose snow avalanches to size one occurring on upper elevation S, SW and even NE facing slopes were reported Wednesday.

Snowpack Summary

Intense recent winds have redistributed snow and created large cornices. The snow surface is now a mix of sastrugi, hard slab and soft slab in open areas.  With the warm temps, slopes receiving direct sun are moistening in the afternoon.  Surface hoar is continuing to form in protected areas too. Below this around 60cm of settled snow rests on a myriad of old surfaces (January 4th interface) that include sun crust on steep south and west facing terrain, surface hoar in sheltered locations at treeline and below and facets everywhere else. Reports indicate that this bond has strengthened over time and is now fairly tight. The overlying slab has also settled significantly. The bond at this interface seems to have strengthened somewhat with time. The overlying slab has also settled significantly.  There are some reports of glide cracks on Mt Fernie, these mysterious phenomena should be given a wide berth.

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