Avalanche Forecast
Issued: Mar 20th, 2014 9:36AM
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
Fair
Weather Forecast
A cool and unstable NW flow should bring light scattered flurries to the region on Friday. A ridge of high pressure builds on Saturday before a weak upper trough crosses the region Saturday night into Sunday morning. Friday: Cloudy with sunny breaks, scattered flurries 1-4cm, freezing level am: surface pm: 700m, ridgetop wind: light NWSaturday: A mix of sun and cloud, mainly dry, freezing level am: surface pm: 800m, ridgetop wind: light variableSaturday Night: Flurries 2-6cm, freezing level: surface, ridgetop wind: light SWSunday: A mix of sun and cloud, mainly dry, freezing level pm: 1200m, ridgetop wind: light W-NW
Avalanche Summary
On Wednesday, we received reports of natural sluffing from steep, south facing terrain in the alpine, likely solar triggered. Two size 1 skier-triggered storm slab avalanches were reported. These occurred on north aspects at treeline and released down around 30cm.We're 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 21st, 2014 2:00PM