Lawinenlagebericht

Kootenay Boundary

Jan 18 – 19, 2013Avalanche Canada
Auf der Karte ansehen
Archiviert · abgelaufen 14 years ago

Lawinengefahr

Sun
Mon
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering
Vollständige Karte öffnen

Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    1–4
    Previous extreme winds out of the W/NW left hard slabs, soft slabs, sastrugi and potentially unstable cornices in their wake. Watch for wind slabs behind midslope features like ridges and ribs. Be alert for wind slabs in unusual locations.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    1–5
    Slopes that didn't slide during last week's avalanche cycle are still of concern. Triggering of this layer is most likely in steep unsupported terrain. Triggering may become more likely in the afternoon on sun exposed slopes.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Saturday: Freezing level starts at valley bottom, rises to 1000m during the day.  Strong ridgetop winds out of the NW.  No precip expected.Sunday: Freezing level starts at valley bottom, rises to 1000m during the day.  Winds start strong out of the NW, backing down to moderate by dinner time.  No precip expected.Monday: Freezing level starts at valley bottom, rises to 1000m during the day. Ridgetop winds mod/strong west.  No precip expected.

Avalanche Summary

No new avalanche observations from Thursday.  On Wednesday numerous wind slab avalanches to size 2 were reported from NE, E and SE facing slopes along with loose wet avalanches to size 1 were also observed on steep solar aspects.

Snowpack Summary

Recent winds have formed hard slabs, soft slabs and sastrugi in open terrain.  We've received reports of hard slabs up to a meter deep in the region. South and West facing slopes have been moistening up during the day with the warm temperatures.  Protected areas are growing surface hoar to 10mm. Under the moist snow and wind slabs the January 4th layer can be found down 50 - 150 cm.  It consists of small facets, surface hoar (up to 12mm) in sheltered treeline and below treeline areas, and a sun crust on steep solar aspects.  When tested, the interface produces the full spectrum of fracture characters from sudden planar to no failure at all.  Needless to say it's quite varied. The midpack is well bonded and strong.

Abgedeckte Regionen