Lawinenlagebericht

South Rockies

Mar 7 – 8, 2015Avalanche Canada
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Archiviert · abgelaufen 12 years ago

Lawinengefahr

Mon
Tue
Hochgebirge
2 · Mässig
Waldgrenze
1 · Gering
Unterhalb
1 · Gering

Kernpunkte

Warm air temperatures with strong afternoon sun may destabilize the upper snowpack on south-facing slopes. Use extra caution on sun exposed slopes during the afternoon.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    1–2
    Ongoing moderate winds from variable directions have created pockets of thin wind slab in exposed leeward terrain features.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely
    Größe
    3–6
    Deeper weaknesses still exist and remain a concern in shallow rocky areas or anywhere the thick near-surface crust is weakening or non-existent, specially north aspects above 2200m.
  • Loose Wet

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Warming temperatures and solar radiation may cause sluffing on steep sun exposed slopes in the afternoon.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Warm and sunny is the theme for the next 3 days. On Sunday, mainly sunny conditions are expected with freezing levels reaching around 2000m. Alpine winds are expected to be moderate from the NW. On Monday, mainly sunny conditions are expected with freezing levels reaching upwards of 2500m. Alpine winds are again expected to be moderate from the NW. Conditions are currently forecast to be the same on Tuesday morning with increasing cloudiness during the afternoon.

Avalanche Summary

On Saturday, wet sluffing was reported from steep sun exposed slopes in the Lizard range. Similar conditions are expected on Sunday.  Human-triggering of old wind slabs also remains possible in isolated areas.

Snowpack Summary

In sheltered areas, up to 10 cm of snow from earlier in the week sits over a previously variable snow surface which was a mix of surface hoar, crusts, wind affected surfaces, and/or dry powder. Ongoing winds have redistributed the new snow in wind-exposed terrain resulting in a highly variable snow surface and the formation of thin wind slabs in leeward features. The most prominent snowpack feature is a thick supportive crust around 10-30 cm below the surface. It extends up to around 2200m elevation. Below this elevation the crust is effectively capping the snowpack, preventing riders from stressing deeper persistent weak layers. In alpine areas where the crust is not present or is less thick, it could still be possible to trigger a deep avalanche from rocky sun-exposed slopes, thin snowpack areas, or with a heavy load (i.e. cornice fall).

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