Lawinenlagebericht

Sea To Sky

Dec 31, 2018Avalanche Canada
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Archiviert · abgelaufen 8 years ago

Lawinengefahr

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

Kernpunkte

The forecast calls for a stable weather pattern in the next few days.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Strong to extreme southerly winds overnight Friday through Saturday have created deep deposits in the alpine and well into tree line.
  • Storm Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Storm snow accumulating over a newly formed weak layer of feathery surface hoar will require time to bond. This layer is likeliest to be found in shady and sheltered areas at tree line.

Confidence

High -

Weather Forecast

MONDAY: Mix of sun and cloud / Light north wind / Alpine temperature -3 CTUESDAY: Mix of sun and cloud / Light northwest wind / Alpine temperature -3 CWEDNESDAY: Flurries / Moderate southwest wind / Alpine temperature 0 C / Freezing level 1500 m

Avalanche Summary

Avalanche activity on Sunday was reported as a few explosives controlled size 1-1.5 storm and windslabs. On Saturday reports indicated several explosives controlled size 2 storm and wind slabs in the alpine and tree line. Some of these avalanches were running on a layer of surface hoar buried around December 26. There was also a report of a size 3 storm slab avalanche that released sympathetically to an avalanche that was set of by an explosive about 30m away.

Snowpack Summary

30-50 cm of recent new snow from the past 7 days potentially sits on a weak layer of feathery surface hoar in the tree line elevation band. Snow amounts will be deepest and touchiest in the lee of terrain features immediately adjacent to ridges.Below 1800 m, around 50 cm of storm snow may not be bonding well to an underlying crust (see here).A weak layer of sugary facets and surface hoar lies around 150 to 200 cm deep in the snowpack. There hasn't been reports of avalanches on this layer for over a week. That being said, this layer may still exist in isolated areas around treeline in some portions of the region.At the base of the snowpack, weak and sugary facets are found below an early-season melt-freeze crust. This weak layer has been the culprit for sporadic, very large avalanches in alpine terrain in the past few weeks. The avalanches have occurred in areas where the ground roughness is very smooth, for example glaciers, firn, and shale/rock slab slopes. An avalanche could be triggered in this layer with a very large trigger, such as a cornice fall.

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