Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 24th, 2017–Feb 25th, 2017

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

Regions

Purcells.

Choose supported terrain and watch for shallow snowpack areas where triggering a large persistent slab avalanche remains possible.

Confidence

High - The weather pattern is stable

Weather Forecast

SATURDAY: Flurries starting in the afternoon with trace accumulations, light west winds, alpine temperatures around -12 C.SUNDAY: Flurries with trace amounts in the north and up to 10 cm in the south, light winds, alpine temperatures around -12 C. MONDAY: Another 2-4 cm by the morning then clearing in the afternoon, light winds, alpine temperatures around -14 C.

Avalanche Summary

On Thursday, a natural size 2.5 persistent slab was reported on a south alpine aspect in the southern Purcells, failing on the February 3rd surface hoar 100 cm deep. A explosive cornice control mission on north aspects generally did not trigger slabs on the slopes below, with one exception of a slab in the recent storm snow. A few small loose dry avalanches were reported in steep terrain. Earlier in the week, there were several large skier triggered avalanches, including a remotely triggered size 2 wind slab near Kimberly, a skier-triggered size 2.5 persistent slab near Golden, and a remotely-triggered size 3 persistent slab near Golden. See here for a MIN report from one of the large avalanches near Golden.

Snowpack Summary

Light flurries over the past few days delivered 10-25 cm of low density snow. Expect to find isolated pockets with thicker wind deposits at higher elevations as well as sun crusts forming on steep south-facing slopes. The recent snow has buried the mid-February interface, which is composed of a thick rain crust up to about 2000 m, sun crusts on steep solar aspects, and spotty surface hoar on shaded aspects. Storm snow from previous weeks is still bonding poorly to the February 3rd surface hoar / sun crust layer, which is now down 60-80 cm. A persistent weakness buried mid January is about a metre deep and the November crust is about 1.5 metres deep. These deep persistent weaknesses still have the potential to wake up and become reactive with human triggers. (See MIN post above).

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.