Avalanche forecast

South Rockies

Mar 25 – 26, 2019Avalanche Canada
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Avalanche danger

Wed
Thu
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
2 · Moderate
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Highlights

Small loose wet avalanches may gather mass, become much larger, and run farther into low angle terrain than expected.

Avalanche problems

  • Loose Wet

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2
    This problem is more likely at lower elevations where there was a weak or no overnight re-freeze. Sunshine and air temperatures above 0 C can rapidly increase the likelihood of triggering loose wet avalanches.

  • Deep Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Unlikely - Possible
    Size
    2–3
    Human triggering of large deep persistent slab avalanches remains possible; especially in rocky, alpine terrain with a shallow or highly variable snowpack depth.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

MONDAY NIGHT: Partly cloudy / Moderate to strong, southwesterly winds / Alpine low -1 C / Freezing level 2000 m.TUESDAY: Mostly cloudy with flurries/ rain in the valleys; 3-10 mm. / Moderate to strong, southwesterly winds / Alpine high -2 C / Freezing level 1700 m.WEDNESDAY: Mix of sun and cloud / Light, easterly winds / Alpine high -1 C / Freezing level 1700 m.THURSDAY: Mix of sun and cloud / Light, easterly winds / Alpine high 0 C / Freezing level 1900 m.

Avalanche Summary

Natural avalanche activity has tapered off, but concern remains for human triggering small loose wet avalanches that quickly gather mass and become dangerous. The link below is a small example of this concern.Last Thursday, there were numerous reports of skiers triggering what started as small loose wet avalanches and then gathered mass and entrained the entire snowpack to the ground running much further than expected, up to size 2. Check out this video from our South Rockies Field Team HERE.

Snowpack Summary

The prolonged warm spell has transitioned sun exposed slopes in the alpine and all aspects at treeline and below towards becoming isothermal (0 C throughout the snowpack). In these areas that have entered spring conditions, the avalanche hazard will fluctuate greatly depending on the strength of the overnight freeze and how quickly the snowpack is warmed up each day. Check out this guide to managing avalanche hazard during spring conditions HERE.In areas that remained more sheltered from the heat, like northerly aspects in the alpine, there may still be a dry snowpack with a well settled slab sitting on weak facets (sugary snow). Human triggering of persistent slabs on this layer may still be possible.Lower down in the snowpack, the base is composed of weak facets. Large, deep persistent slab avalanches are most likely in rocky, alpine terrain where there is a shallow or highly variable snowpack depth. They would likely require a large trigger such as a cornice fall, snowmobile, or a group of people standing in the same spot.

Regions covered