Lawinenlagebericht

Northwest Inland

Feb 5 – 6, 2013Avalanche Canada
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Archiviert · abgelaufen 14 years ago

Lawinengefahr

Thu
Fri
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
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Kernpunkte

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–5
    New snow and strong shifting winds have built wind slabs that are likely found behind terrain breaks such as ridges and ribs.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–6
    Buried beneath the new snow sits a surface hoar/crust/facet weakness. This may be sensitive to rider triggers in steeper sheltered terrain or over convex rolls, especially at treeline and below treeline elevations.

Confidence

Fair - Due to limited field observations

Weather Forecast

Wednesday: Expect mostly cloudy skies with a chance of flurries. Winds should be light southerly and alpine temperatures should reach -7.Thursday: We should see a mix of sun and cloud with winds turning westerly then northwesterly and strengthening. Very isolated flurries are possible. Alpine temperatures should reach around -8.Friday: Clouds return with a slight chance of flurries. Winds settle back to westerly and increase to moderate values. Expect temperatures around -7.

Avalanche Summary

A natural cycle has passed with windslab avalanches at treeline and in the alpine up to size 2.5 and loose wet sluffing at lower elevations.

Snowpack Summary

Up to 40cm of recent storm snow has fallen in the past 72 hrs. Consistent southwesterly winds have maintained snow transport, and many lee zones show layers of windslab over windslab. The deepest storm interface (from the very beginning of this storm cycle) includes a huge variety of old surfaces from facets to crusts and isolated pockets of surface hoar (sheltered treeline and below treeline). There is very limited information with regards to this interface, with the only results suggesting reactivity in sheltered, shady treeline and below treeline slopes (likely associated with the preserved surface hoar pockets). I would stress the importance of digging down to find and test weak layers. A cautious and curious approach is critical.At low elevations (below 800m) the recent storm snow is still moist below the surface. Wet slabs at low elevations may still be possible in steep convex features.The strong mid-pack overlies a weak base layer of facets/depth hoar. Triggering of this basal weakness may still be possible from thin spots, rocky outcrops or under the weight of larger triggers such as cornice fall.

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