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Avalanche Forecast

Archived

Jan 10th, 2014–Jan 11th, 2014

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
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.

Regions

Sea To Sky.

Confidence

Good

Weather Forecast

Overnight and Saturday: Heavy snowfall occurring overnight and throughout Saturday / Moderate southwest wind (with extreme gusts) / Freezing level at 1100mSunday: Light snowfall / Moderate to extreme west winds / Freezing level at valley bottom rising to 1300mMonday: Light snowfall / Moderate to extreme southwest winds / Freezing level at 1300m

Avalanche Summary

On Thursday, numerous wind slab avalanches to size 1.5 were observed in alpine terrain. A size 2 deep persistent slab avalanche was reported on Blackcomb on Wednesday. This slide was accidentally triggered by a snow cat and failed on a weak facetted layer near the ground. Check out Waynn Flann's avalanche blog for photos and more information. This avalanche highlights the potential for large and deep avalanches in many areas on the South Coast. Heavy loading Friday night and Saturday will most likely trigger full depth avalanches in some places.

Snowpack Summary

Around 15-30 cm of new snow has fallen in the last few days and may overlie surface hoar in sheltered terrain. Ongoing moderate to strong southwest winds have formed touchy wind slabs in exposed lee terrain and cross-loaded features. The cold temperatures from early December have left weak faceted crystals that seem to be variably reactive. In higher elevation terrain where the snowpack was deeper, the facets likely co-exist with a crust in the mid pack. In lower elevation terrain or in shallow, rocky areas of the alpine, the facets are most likely more widespread and may exist down near the ground. Either way, the "wait 48 hours and you're good" Coastal mantra does not apply as these conditions are likely to persist for some time, and will probably become reactive with forecast snowfall.Early season riding hazards such as rocks, stumps and logs are lurking below the surface in many areas. In glaciated terrain open and poorly bridged crevasses are everywhere.

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.