Avalanche Forecast
Issued: Mar 21st, 2014 9:45AM
The alpine rating is Storm Slabs, Persistent Slabs and Deep Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Good
Weather Forecast
A weak frontal system should bring light precipitation to the interior midday Saturday. A ridge of high pressure builds in its wake on Sunday and should persist through Monday. The next system is expected for Tuesday.Saturday: Light precipitation 3-5mm, freezing level am: surface pm: 800m, ridgetop wind light SW-WSunday: Mostly sunny, dry conditions, freezing level am: 400m pm: 1200m, ridgetop wind light W-NWMonday: A mix of sun and cloud, dry conditions, freezing level am: 500m pm: 1500m, ridgetop wind light SW-W
Avalanche Summary
Reports from Thursday include numerous natural and skier triggered avalanches up to size 2.5. These occurred on all aspects and elevation bands, and typically released down 30-40cm. One avalanche stepped down to the early-March layer. In the N. Columbia region, one avalanche stepped down to the early-February layer.Generally, we are still seeing relatively small inputs, like periods of strong winds or brief sunny breaks, trigger deeper persistent slab avalanches. Many of these events have occurred on southerly aspects from slopes in the alpine or at treeline. Extra caution is advised when the sun is out.
Snowpack Summary
30-60 cm of recent storm snow sits on the mid-March interface, which is commonly described as a sun crust/surface hoar sandwich. Recent snowpack tests show variable results on this weakness, with mostly hard shears where the storm snow overlies surface hoar. Periods of gusty SW-NW winds have redistributed some of the new snow forming soft wind slabs in exposed lee terrain.The early March persistent weak layer, which is a crust mixed with facets or surface hoar in places, is now down around 80-120 cm. This layer has been most reactive on southerly aspects. The mid-February crust/facet/surface hoar layer is widespread throughout the region, but the depth varies significantly. It still producing sudden "pops or drops" results in snowpack tests where it is less than 150 cm deep. The biggest concern with this interface is being able to trigger it where it is less deep and having it propagate into thick snowpack areas producing very deep and large avalanches. Cornices are also large and fragile at this time and could pop off during sunny breaks.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Deep Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Mar 22nd, 2014 2:00PM