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

Mar 8th, 2014–Mar 9th, 2014

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.
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.

More snow/rain=More Danger!Forecasted snowfall/rain will be higher in the south of the region. Danger ratings reflect the zones with higher precipitation amounts.South Rockies Blog

Weather Forecast

The large moist pacific system is poised to reach the South Rockies by Saturday evening bringing increased winds from the south and moderate to heavy precipitation overnight. The southern areas of the forecast region (Elk Valley South and Flathead) will see more precipitation than the north as the system is sticking close to the US/Canada border. Sunday will see continued rain and snow, with a possible dip in the freezing levels as the frontal system passes later in the day. Quieter, spring like weather should prevail for Monday, Tuesday.Ovn Sat: 2-5mm north/15-20mm in the south, with strong south winds as the system arrives. Freezing levels 1600-1800mSunday: 5-20mm with moderate west winds with strong gusts and freezing levels up to 2100m.Monday: No significant precipitation, sunny breaks with light west winds and freezing levels 1700-1800m

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 as danger ratings rise on Sunday. Avalanches in the region have the potential to run full path. As an example we got a report of an avalanche hitting the road during the day on Friday on Hartley Lake Road.Two recent avalanches on east aspects, size 2.5-3 were noted by the field team and other observers in the Crowsnest pass on Friday.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, while other areas like the Crowsnest, had dry snow below treeline under the influence of colder air. 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 . Forecasted new snow and rain, combined with warm temperatures, will likely create another storm slab avalanche cycle by Sunday. Moderate to strong SW winds will continue to create windslabs in alpine lee features and contribute to the already significant cornice growth..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 weakness. 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.