Avalanche Forecast

Archived

Mar 19th, 2014–Mar 20th, 2014

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Regions

Cariboos.

We should see sunny breaks over the next few days. Brief periods of solar radiation could be enough to trigger stubborn persistent slabs or cause cornice failures. Conservative route selection is crucial at this time.

Confidence

Fair

Weather Forecast

Thursday: Cloudy with flurries and sunny breaks – up to 5 cm. The freezing level is around 600-800 m and ridge winds are light gusting moderate from the NW. Friday: A mix of sun and cloud. The freezing level is around 600 m and ridge winds are light from the NW. Saturday: Mainly cloudy with sunny breaks and a chance of flurries. The freezing level is near valley bottom. Ridge winds are light.

Avalanche Summary

We continue to see large natural avalanches stepping down to the deeply buried persistent weak layers. On Tuesday there was one report of a size 2.5 remotely triggered avalanche where a group of skiers felt a massive whumpf at the top of a slope and realized that they triggered an avalanche on an adjacent slope almost 500 m away. On Monday there were also a couple reports of large slab avalanches. Some of these were on southerly aspects and likely involved buried sun crusts (early March interface) with avalanches up to Size 3. One was accidentally skier triggered from a Northeast aspect at treeline and likely released on the mid February weak layer. A group of snowmobilers triggered a large avalanche not far from Blue River on March 14 resulting in one fatality. Some information is available here.

Snowpack Summary

Around 30-40 cm of recent storm snow has fallen in the past few days. There may be a variety of layers within the storm snow from thin sun crusts, to graupel balls, and maybe even recently buried surface hoar from brief clearings overnight. Also, expect fresh wind slabs in exposed lee and cross-loaded terrain. This new snow now sits on a surface hoar and/or sun crust layer. Some recent snowpack tests give moderate "pops or drops" shears on the interface between the recent storm snow and previous surface. A couple other notable persistent weaknesses remain a concern in the mid-snowpack. Another surface hoar/sun crust combo buried in early March is now down around 60-80 cm. The February 10th surface hoar/facet/crust combo is 90cm - 150cm below the snow surface and widespread throughout the region. Surface avalanches in motion and cornice fall have the potential to initiate an avalanche on this deeply buried weak layer. The mid and lower snowpack remains weak and facetted in areas with a relatively shallow snowpack.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.