Bollettino valanghe

Northwest Inland

Dec 17 – 18, 2011Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 15 years ago

Pericolo valanghe

Mon
Tue
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2
    Wind slabs have developed on lee and cross-loaded terrain in the alpine and at treeline. Expect further development with monday's forecast weather
  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–2
    Expect general storm slab activity on a variety of aspects as the new snow gains cohesion and creates more load on buried weak layers

Confidence

Fair - Intensity of incoming weather is uncertain on Monday

Weather Forecast

Mostly clear skies are forecast for sunday morning with freezing levels at or near surface. Late in the day another frontal system will hit the region bringing 10-15cm of snow overnight and throughout monday. Moderate to strong southwest winds and freezing levels of 900m will accompany this system.Tuesday calls for light to moderate snowfall in the morning, cooler temperatures and reduced westerly winds.

Avalanche Summary

No new avalanches have been reported. This may speak more to lack of reports from the field than actual avalanche conditions. Any information (professional or recreational) from the field is highly appreciated. Please send your observations to [email protected].

Snowpack Summary

About 15 centimetres of new snow and surface hoar crystals are sitting on the less recent 20cm of storm snow which fell earlier in the week. This storm snow we received earlier this week sits on a variety of old weak snow surfaces including surface hoar, melt-freeze crusts and facetted snow. For the most part all aspects between 900m-2000m have a hard melt freeze crust. This crust is widespread and is lingering in most start zones. This is the layer of concern at the moment. Above this crust surface hoar (feathery crystals) and facets (sugary crystals) may be preserved. The recent winds in the alpine seem to have destroyed the surface hoar in exposed areas in the alpine eliminating that problem but creating a wind slab problem. In short, the upper snowpack is variable and a cautious approach is required as new slabs continue to form over the buried weak layers. The midpack seems to be well settled and strong.

Regioni coperte