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 14th, 2013–Mar 15th, 2013

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

Regions

Sea To Sky.

Confidence

Fair - Freezing levels are uncertain on Friday

Weather Forecast

Synopsis:  The true pineapple breaks down Friday and a more zonal flow builds in its place which opens the door to a series of weak systems. Friday:  Freezing Level 1300m.  Precip: 2-5mm Wind: Light, SESaturday:  Freezing Level 900m.  Precip: 4mm Wind: Moderate SW gusting to StrongSunday: Freezing Level 1100m in the afternoon, dropping to the surface overnight.  Trace of precip.  Wind: Light, NE

Avalanche Summary

Quite a few observations of a natural cycle to size 2.5 at upper elevations on Wednesday were received.  Both slab and loose snow avalanches were running on all aspects at the new/old snow interface down around 50 cm in depth.  It's no surprise that explosive control work in the region also produced avalanches to size 2.5 on most aspects as well. 

Snowpack Summary

The storm has delivered around 50 cm of heavy snow at upper elevations as of Thursday morning and another 15 - 25 are expected this afternoon and evening. Strong southerly winds in the alpine have created slabs on N - E facing slopes that may be up to a meter in depth.  At treeline the storm snow is a messy configuration of dry snow, moist snow, rain soaked snow and even the occasional thin crust.  As this interface cools in the coming days the ski quality may be less than premium. This new snow is bonding poorly to the previous snow surface, which includes faceted snow, surface hoar, and/or a crust, but is most concerning where surface hoar is sitting on a crust on previously sun-exposed sheltered treeline slopes. Around a metre below the snow surface is a layer surface hoar buried on February 20th. Although this layer has a history of producing large avalanches, triggering this layer has now become difficult, and would most likely require a very large trigger on a steep, unsupported slope. Below this interface, the snowpack is strong and well settled.

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.