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Avalanche Forecast

Archived

Mar 7th, 2014–Mar 8th, 2014

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

South Rockies.

Check out the South Rockies Blog and Forecaster Blog for more information on current snowpack and avalanche conditions.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

The ridge of high pressure shifts inland by Friday night pushing out the last of the patchy moisture. Generally dry conditions with some sunny breaks expected for Saturday morning, but clouds and increased winds will return by the evening as the large pacific frontal system approaches. Moderate to heavy precipitation is expected overnight on Saturday and Sunday morning, with a chance of freezing levels dropping slightly sometime on Sunday with the passage of a cold front.Overnight Friday: Trace of new snow, cloudy, moderate south west winds, with freezing levels between 1200-1400m.Sat: Trace of new snow for the day, increasing west winds (gusting to strong) by late afternoon. Heavy snow/rain expected overnight on Sat with freezing levels 1800-1900m.Sun: Morning snow/rain, heavy at times, easing during the day, moderate (gusting to strong) south west winds, freezing levels 1900-2100m, but possibly dropping later in the day.Mon: Trace of precipitation possible, light winds, freezing levels 1700m

Avalanche Summary

Avalanches in clearcuts, road banks, lower angle terrain and non obvious avalanche paths continue to surprise backcountry enthusiasts throughout the region so consider them carefully in your travel plans.Two recent avalanches on east aspects, size 2.5-3 were noted by the field team in the Crowsnest pass today.In the Harvey Pass area there was a widespread natural cycle on Thursday with some avalanches up to size 3. Most avalanches are failing at the storm snow interface, but some are initiating or stepping down to the February 10th persistent weak layer, even in surprisingly low angle and gladed terrain.There was a report of a large avalanche in Thursday's cycle hitting the grooming about 4km before the Rolling Hills cabin near Fernie.On Thursday the South Rockies team reported a size 2.5 avalanche out of a north facing chute near Grave Lake that left 6 meters of debris on a logging road, blocking their return to the trucks.

Snowpack Summary

Some areas of the South Rockies (Elk Valley South and Flathead) received Thurday's precipitation as significant rain event below 1500m-1700m. In areas above 1600m there is approximately 40-70cm of new storm snow sitting on top of the March 2 interface consisting of surface hoar, facets or a crust depending on your aspect and elevation . Moderate to strong SW winds combined with the new snow have created windslabs in lee features and have likely contributed to cornice growth at upper elevations.The mid pack still contains a layer of facets and/or surface hoar that is now down between 70-180cm depending on your location in the South Rockies. It is still showing good fracture character on snowpack tests, suggesting that it may be possible for storm slabs to step down to this persistent weak ness.  Check the South Rockies Blog for the latest snowpack discussion.

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.

Wet Slabs

Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.

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.