Lawinenlagebericht

South Rockies

Feb 27 – 28, 2019Avalanche Canada
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Archiviert · abgelaufen 8 years ago

Lawinengefahr

Fri
Sat
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
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Kernpunkte

Recently formed wind slabs and wind-affected snow may quickly be hidden under a thin cover of flurries falling through Thursday. Expect a more reactive snowpack in areas where winds pick up and 10 cm snowfall accumulates.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    5-10 cm flurries falling with wind through Thursday will build new wind slabs with deeper and more sensitive deposits in wind-loaded terrain. Harder, recently formed, wind slabs may be hidden under a thin cover of new snow.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–2.5
    A weak layer of surface hoar is buried around 40 to 80 cm, which is best preserved in shaded and sheltered areas between 1600 m and 1900 m.

Confidence

Moderate - Wind effect is extremely variable

Weather Forecast

WEDNESDAY NIGHT: Clear with cloudy periods. Alpine temperatures near -12C. Ridgetop winds 10-15 km/h from the east.THURSDAY: Cloudy with scattered flurries, 5-10 cm. Alpine temperatures near -12C. Ridgetop winds 10-20 km/h from the southeast.FRIDAY: Mainly cloudy with isolated flurries, trace to 8 cm. Alpine temperatures near -19C. Ridgetop winds 15-25 km/h from the east.SATURDAY: Sunny with cloudy periods. Alpine temperatures near -22C. Ridgetop winds 10-15 km/h from the east.

Avalanche Summary

On Monday, small (size 1) wind slabs were reactive to skier traffic, and an isolated natural wind slab avalanche event up to size 2.5 likely occurred overnight Monday.Several large (size 2) wind slabs were triggered with explosives control in the Castle area on Friday after a bout of strong to extreme southwest winds. Slab depths ranged from 20-60 cm.A MIN report from Grizzly Peak in the Elkford area last Thursday describes a persistent slab failing on the mid-January persistent weak layer as a ski touring group ascended a steeper slope near treeline. See the report here.Also last Thursday in adjacent Waterton National Park, a recent large (size 2) deep persistent slab avalanche was observed. It occurred on a steep feature below treeline that was noted for its thin snowpack and for being reverse loaded by winds.

Snowpack Summary

Widespread wind affect has smoothed alpine terrain and loaded lee features. Harder wind slabs are found in more exposed terrain and higher elevations, softer wind slabs have formed in more sheltered areas.Below this stack of wind-affected snow, a weak layer of surface hoar or faceted grains buried mid-January is down 40 to 80 cm. It is found on shaded and sheltered slopes and is most prominent between 1600 m and 1900 m but has been found up to 2200 m. It may overly a melt-freeze crust on south aspects. Recent avalanche reports and snowpack test results suggest that this layer remains reactive to human triggers.The bottom half of the snowpack is composed of weak and sugary faceted snow crystals.

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