Lawinenlagebericht

Northwest Inland

Jan 15 – 16, 2015Avalanche Canada
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Archiviert · abgelaufen 12 years ago

Lawinengefahr

Sat
Sun
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering
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Kernpunkte

Lack of recent avalanche activity indicates we haven't seen the loads necessary to trigger buried weak layers. Conservative route selection is still essential to staying safe while the snowpack bonds.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Forecast winds with new snow will load lee slopes in the next little while. Be aware of wind-loaded pockets that might fail with rider loads.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–6
    This weakness is widely variable in depth and seems to be mostly around tree-line and below . It could be triggered by a small wind-slab avalanche or the weight of a snow machine.

Confidence

Fair - Due to the number and quality of field observations

Weather Forecast

A fast-moving cold front arrives on the North Coast Thursday afternoon bringing more precipitation. Rain at lower elevations and snow above 1500 metres. Freezing level should drop to 700 metres late Thursday night, or early Friday morning. The Inland region should see 2 to 5 cm of snow on Thursday, and 5 to 10 cm on Sunday.

Avalanche Summary

No reports of avalanche activity in the region yesterday, but further west there have been reports of large natural avalanches on N and NW facing slopes around 1800m.

Snowpack Summary

Strong South winds are building wind-slabs, generally depositing snow on N and NE aspects. A rain crust is still out there up to 1600m and melt freeze crust to 1850m. Keep in mind a surface hoar layer reported to be 15 to 20cm below the surface in areas protected from the wind. We're watching the December crust, but we haven't seen any activity on it recently, most likely because it hasn't received a significant load on it. Near the base of the snowpack is a November crust-facet combination that could remain problematic for some time.

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