Bollettino valanghe

Waterton Lakes

Dec 9 – 12, 2014Parks Canada
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Archiviato · scaduto 12 years ago

Pericolo valanghe

Tue
Wed
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

Warming will cause some deterioration in both the snowpack and travel conditions especially for Wednesday. Below treeline travel off of trails is not recommended due to poor coverage.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    Thin windslabs can now be found at treeline. This slabs are thin and very localized and are easy to stumble into as they appear mid slope in front of you. With the warmer temps expected these slabs may become more sensitive before they improve.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    1–2
    These slabs taper radically with elevation and are sitting on a thick crust. Large slides resulted from failures in the recent storm snow over the crust that extends to around 2300m. These slabs may become easier to trigger with the expected heating.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    1–3
    At high elevations cooler temps have only allowed thin crusts to form above the weak November Facets which may remain a possibility for triggering for some time. Use caution TL and above especially in thin or variable areas.

Weather Forecast

The freezing level is expected to continue rising Tuesday reaching  near mountain top with about 10mm of rain forecast. Freezing levels look to return to Little Prairie Wed and hopefully the 10mm of precip forecast for Wed night arrives as snow.

Snowpack Summary

Suncrusts forming steep South slopes. Wind effect found in open areas treeline and above. Mid-Nov facets sit on 30cm of crusts formed early in November at treeline and above. Below 2200m, rain at the start of the storm on Nov 26 created a crust over the facets or melted them. The slab above these layers grows with elevation from 30 to 100 cm.

Avalanche Summary

There is some small solar activity occurring on steep solar slopes especially around black bodies. It is easy to trigger wind slabs in specific locations. We continue to find further evidence of the widespread cycle on November 28 but have seen no recent activity on these layers.

Confidence

Due to the number and quality of field observations

Regioni coperte