Lawinenlagebericht

South Coast

Jan 20 – 21, 2015Avalanche Canada
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Archiviert · abgelaufen 12 years ago

Lawinengefahr

Thu
Fri
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering

Kernpunkte

Dry and mild conditions should persist for at least one more day. Be alert to changing conditions from daytime warming and sunshine.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–4
    Watch for pockets of reactive wind slab on steep convex shaped slopes near ridge top. Cornices could also become weak if the sun is out and temperatures warm on Wednesday.
  • Loose Wet

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    If the sun hangs around for one more day we could see more loose wet activity on sun-exposed slopes during the day. 

Confidence

Good

Weather Forecast

Synopsis: The ridge of high pressure will maintain dry and mild conditions on Wednesday. Freezing levels could climb to a little over 1500 m and ridge winds remain light. Expect more cloud with a chance of flurries on Thursday. The freezing level should drop back to 1000m but some areas could still see an above freezing layer in the alpine. We could see periods of moderate SW winds. The next system appears to arrive on Friday bringing moderate precipitation, rising freezing levels, and strong SW ridge winds.

Avalanche Summary

Several natural wind slab avalanches were reported during and at the end of the recent storm (ending early Monday). On Monday one natural size 3 avalanche and one size 1.5 accidentally triggered avalanche were reported from the South Chilcotin Mountains. These were both wind slabs on northerly aspects near ridge top. Info is limited from the Coquihalla and other southern areas but one observer noticed the deposits of several natural size 2-2.5 slides from the road.

Snowpack Summary

Recent snowfall amounts vary from north to south with an average of 25-35 cm of new snow near the Duffey Lake Road and 40-60 cm in the Cascades (Coquihalla and Allison Pass). Strong W-SW winds created deep and dense wind slabs in wind-affected terrain. The fresh storm and wind slabs overlie a hard crust and/or surface hoar layer. The bond to the crust could be somewhat variable but many observers report a good bond. Where surface hoar is present (possibly above the crust) the storm slab has been more reactive to ski testing on steep unsupported features. Deeper snowpack weaknesses are still on our radar, but seem to be dormant for the time being.

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