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Avalanche Forecast

Archived

Apr 15th, 2015–Apr 16th, 2015

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

Regions

South Coast.

Tricky winter conditions exist at higher elevations. Solar radiation and rising temperatures are forecast and avalanche hazard can rise quickly. Use a conservative approach and watch for signs of instabilities.

Confidence

Poor - Due to the number of field observations

Weather Forecast

The current wintery weather pattern begins to change as a dominant upper ridge sets up over the province. The next frontal system seems to just skirt north of the South Coast region bringing little to no precipitation. Thursday and Friday will see a mix of sun and cloud. Ridgetop winds will be moderate  from the west and freezing levels will rise to 2700 m. Saturday will be mostly sunny with alpine temperatures rising to +6.0 degrees with light ridgetop winds. Freezing levels will remain at 2600 m. The ridge  will remain stationary until Wednesday bringing warm air and sunny skies.

Avalanche Summary

No reports of avalanche activity from yesterday. This is most likely as a result of few field observations. I suspect wind slab activity with new loading and strong winds. Strong solar radiation and warming expected on Thursday will likely initiate a natural avalanche cycle. Watch overhead hazards like cornices.

Snowpack Summary

Anywhere from 20 to 50 cm of recent storm snow sits on a variety of old surfaces including crusts, surface hoar and facets that were buried April 10th. Moderate to strong south west winds are redistributing the storm snow into wind slabs on leeward slopes and terrain features. The mid-March persistent weak layer of facets on a crust is now approximately 50-100 cm down. This remains a concern in the region due to its potential to produce very large avalanches. There may be a low probability of triggering this layer, however; if it is triggered the consequence would be high. Large looming cornices may become weak with solar radiation and daytime warming. If a cornice fails it could trigger a large avalanche from the slope below.

Problems

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.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.