Lawinenlagebericht

South Rockies

Dec 27, 2017Avalanche Canada
Auf der Karte ansehen
Archiviert · abgelaufen 9 years ago

Lawinengefahr

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

Kernpunkte

Winds are expected to increase, so watch for slopes getting loaded with blowing snow.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    1–2
    Expect slabs at higher elevations where wind has formed hard deposits of snow on the downwind sides of ridges and gullies.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    A weak layer composed of surface hoar and/or crusts is buried 30-60 cm below the surface. Triggering an avalanche on this layer is possible in areas where the snow has settled into a cohesive slab.

Confidence

Moderate - Wind speed and direction is uncertain

Weather Forecast

WEDNESDAY: Mix of sun and cloud, strong west winds, treeline temperatures around -20 C.THURSDAY: Cloudy with flurries starting in the afternoon, strong west winds, treeline temperatures around -17 C.FRIDAY: 5-20 cm of low-density snow, strong west winds, treeline temperatures around -17 C.

Avalanche Summary

Limited reports suggest triggering slab avalanches remains possible. Two skier triggered avalanches have been reported east of the divide the past few days. One was a small wind slab triggered in a steep gully and the other was a larger persistent slab (size 2) triggered low on a slope that propagated up and across the slope on a 50 cm deep crust. The later highlights the potential for persistent slab avalanches to have wide propagations.

Snowpack Summary

Cold temperatures are preserving fresh snow from the past week, with up to 60 cm in southern and eastern parts of the region and 30 cm in the Elk Valley. The snow has been deposited into harder wind slabs in exposed terrain, but remains low density in sheltered areas. The main question in the snowpack surrounds the layer sitting beneath the new snow. The layer includes crusts on solar aspects and large feathery surface hoar crystals in sheltered terrain at and below treeline. The distribution of the layer, as well as the properties of the snow above it, is variable. The most suspect areas are where the wind has blown extra snow above this layer and on slopes with preserved surface hoar.Two crusts that were buried near the end of November can be found lower in the snowpack. A third crust from the end of October exists near the base of the snowpack. Recent testing on these crusts has not produced significant results.

Abgedeckte Regionen