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Avalanche Forecast

Archived

Feb 16th, 2015–Feb 17th, 2015

Alpine
Natural avalanches possible, human triggered probable.
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

Little Yoho.

http://www.pc.gc.ca/apps/scond/Cond_E.asp?oID=19299&oPark=100092

Conditions in Little Yoho will likely improve more quickly than further east. However, poor ski conditions at lower elevations have prevented good recent observations from this area. Choose conservative terrain and gather your own snowpack info!

Weather Forecast

A ridge of high pressure is sitting above us. We can expect pleasant spring weather on Tues and Wed with light alpine winds, cool overnight temperatures (-10/ -15) and minimal solar effect on the snowpack despite the sunny skies. Winds should pick up to moderate from the West on Wed PM and we may see some light snow (5-10cm's) overnight Wed.

Snowpack Summary

Above 2000m, soft wind slabs have formed on many different aspects. 60-80 cm of settled storm snow at treeline and above overlies a generally settled snowpack. Some snow pits have found facets at this storm snow interface. Below 1800m a breakable surface crust exists on all aspects which becomes supportive and stronger at lower elevations.

Avalanche Summary

No new avalanches were reported today in Little Yoho, however our field teams haven't had good observations from this area for a week or so. Although not in the Little Yoho region, on Saturday, a natural avalanche cycle to size 3 occurred in the Bow Summit area. Click here for photos of these events.

Confidence

Due to the number and quality of field observations

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.