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Avalanche Forecast

Archived

Nov 19th, 2011–Nov 20th, 2011

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Sea To Sky.

This bulletin is based on limited data. Local variation in conditions and danger levels are likely to exist. To produce more accurate forecasts, we need information. Please send an email to [email protected].

Confidence

Poor - Due to limited field observations

Weather Forecast

Sunday: Expect clouds to build and winds to shift to southwesterly and remain light. Treeline temperatures could reach -5. Chance of flurries late in the day. Monday & Tuesday: Increasing snowfall amounts (up to 50cm) with winds building to strong southwesterlies. The freezing level may climb to 1500m on Tuesday.

Avalanche Summary

Avalanche activity has slowed down with the colder temperatures, but recent reports include wind slab avalanches up to Size 2.5 failing on the crust/surface hoar combo that was buried November 9. Some slabs were up to a metre deep and pulled back into low angled terrain on ridges showing incredible propensity for propagation. The critical elevation band for the crust/surface hoar combo is between 1800 and 2050m.

Snowpack Summary

There has been limited new snow in the past couple of days and the colder temperatures have tightened up the storm snow instabilities. The snowpack sits at about 100cm in sheltered locations at treeline, with deeper, wind deposited pockets in the alpine and around ridgeline features. A rain crust, buried November 9 is prominent between 1800m and 2050m and has surface hoar crystals either above, within or slightly below it. This crust/surface hoar combo is buried 40 to 70cm and is the deeper layer of concern.Another 20-30cm of upside-down storm snow brings total snowpack depths up to a metre or so in sheltered treeline areas, but expect to find much deeper pockets of wind-blown snow immediately down-wind of terrain features and ridge crests. A thick rain crust from last week is 70 or 80 cm off the ground at treeline and lower alpine elevations, with facets above and below in some locations. Above that is a buried layer of surface hoar that formed during the clear weather over the weekend. These weaknesses now have a sufficiently thick and cohesive slab to produce avalanches in most areas and they have all the characteristics of an avalanche problem that could persist for extended periods.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.