Lawinenlagebericht

South Rockies

Jan 17, 2017Avalanche Canada
Auf der Karte ansehen
Archiviert · abgelaufen 10 years ago

Lawinengefahr

Tue
Wed
Hochgebirge
3 · Erheblich
Waldgrenze
3 · Erheblich
Unterhalb
2 · Mässig

Kernpunkte

A sudden change in weather can have surprising effects on the snowpack. Conservative terrain use is key.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Although there's not much new snow in the forecast, strong winds will transport loose surface snow and form touchy wind slabs on lee features.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    2–3
    Rapid warming will increase the likelihood of triggering persistent weak layers that have been lingering deep in the snowpack.

Confidence

Moderate - Freezing levels are uncertain on Tuesday

Weather Forecast

TUESDAY: Scattered flurries with up to 5 cm of new snow, extreme southwest winds, freezing levels rising to 1500 m and likely higher on the eastern slopes.WEDNESDAY: Scattered flurries with up to 5 cm of new snow, strong southwest winds, freezing levels rising to 1700 m and likely higher on the eastern slopes.THURSDAY: Clearing with isolated flurries, strong southwest winds, freezing level around 1500 m.

Avalanche Summary

On Sunday, a natural size 1.5 wind slab was reported on a northeast aspect. An MIN report from Waterton Park on Friday shows a large size 3 deep persistent slab avalanche triggered by a smaller wind slab on a feature with highly variable snow depths. Although an isolated event, this avalanche highlights the possible consequence of our tricky persistent slab problem, especially with the incoming change of weather.

Snowpack Summary

Increasing winds are causing widespread wind affect in exposed alpine and treeline terrain and forming reactive wind slabs on lee features. The mid pack is quite variable throughout the region and the structure depends on snow depth. In deeper snowpack areas, the snowpack appears to be well settled and right side up with isolated concerns for the mid-December facet layer found 50 to 80 cm deep. In shallow snowpack areas and lower elevations, the snowpack is heavily faceted and there are concerns for the mid-December weak facet layer as well as weak basal facets. If a persistent slab is triggered from thinner snowpack areas it may release on the basal facets resulting in a full depth avalanche. Triggering these deeper weak layers will become more likely this week as warm temperatures soften the overlying slab.

Abgedeckte Regionen