Lawinenlagebericht

South Coast Inland

Feb 8, 2017Avalanche Canada
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Archiviert · abgelaufen 10 years ago

Lawinengefahr

Wed
Thu
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig

Kernpunkte

Storm slabs will likely be most reactive in wind effected terrain. Avoid slopes where the snow feels stiff or slabby.

Lawinenprobleme

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–3
    This problem is more prevalent in the far north areas of the region and is a low likelihood, high consequence scenario that will need to be monitored as snow loads increase.
  • Storm Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Lingering storm slabs may remain reactive to human triggers.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Wednesday: Mostly cloudy / Light, southeasterly winds/ Freezing sea level.Wednesday night: 10-15 cm new snow / Light to moderate, southerly winds / Freezing level sea level.Thursday: 20-25 cm new snow / Strong, southwesterly winds / Freezing level 800m.Friday: Mix of sun and cloud / Moderate, westerly winds / Freezing level 800 m.

Avalanche Summary

A skier triggered size 1 persistent slab avalanche on a small convex feature southest of Bralorne. The weak layer was down 50 cm and suspected to be the surface hoar/facet layer that was buried in mid-January. This layer has been largely dormant but may become active in isolated locations where the weak layer is well preserved. Continue to dig down and test this weak layer to monitor its reactivity.

Snowpack Summary

35-50 cm(lower amounts in the north) of recent storm snow has buried a wide variety of old snow surfaces including stiff wind slab or wind effected snow at upper elevations, sun crust on steep southerly slopes, surface hoar and surface facets in sheltered locations. The mid-January surface hoar and facet interface is now buried 50-80 cm and the mid-December facets down 90-120 cm remain a concern especially in shallower snowpack areas like the Duffey, Hurley and/ or South Chilcotins. These deeper weaknesses warrant monitoring especially through periods of more load. In southern areas (Coquihalla), the lower snowpack is reportedly well settled(stronger), than it is to the north.

Abgedeckte Regionen