Avalanche Forecast
Issued: Mar 17th, 2015 9:16AM
The alpine rating is Storm Slabs, Loose Wet and Deep Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Fair - Timing, track, or intensity of incoming weather system is uncertain
Weather Forecast
Light precipitation can be expected Tuesday overnight into Wednesday morning. There is currently some model uncertainty regarding amounts but the region could see 2-10mm with freezing levels around 1500m. By Wednesday afternoon the clouds should break and sunny periods are possible. Freezing levels should reach around 2000m Wednesday afternoon and alpine winds should be moderate from the NW. On Thursday, a warm storm system reaches the south coast. There is currently quite a bit of uncertainty regarding the timing and track of the system into the interior regions. For the South Rockies region, it is currently looking like unsettled conditions for Thursday with mainly cloudy conditions. Freezing levels should again reach around 2000m and alpine winds may be strong from the SW to W. On Friday, light precipitation is possible but amounts are uncertain. Freezing levels may climb to over 2500m.
Avalanche Summary
We haven't received any reports recently but this likely speaks to a lack of observers. In the Lizard region, a natural avalanche cycle up to size 2.5 was reported with slabs up to 80cm thick. Similar activity is expected to have occurred in the South Rockies Region. On Wednesday, human-triggering of storm slabs remains a major concern, especially in the alpine. Wind-loaded features and steep, unsupported slopes are the most likely areas to trigger an avalanche. Loose wet avalanches are possible during the heat of the afternoon, especially on sun-exposed slopes.
Snowpack Summary
Heavy rain (up to 60 mm) on Saturday soaked the snowpack. On Sunday the rain changed to snow as the freezing levels slowly dropped. Heavy snowfall (up to 50cm) combined with strong southwest winds developed new storm slabs on all aspects in the alpine and at treeline. The thick mid-February crust was 10-30cm below the surface before the recent storm and extends up to around 2200m elevation. Below this elevation the crust is effectively capping the snowpack, preventing riders from stressing deeper persistent weak layers. In high alpine areas where the crust is not present or is less thick, dormant persistent weak layers may still be lingering and could wake-up with heavy loading or strong warming.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Loose Wet
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Deep Persistent Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Valid until: Mar 18th, 2015 2:00PM