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 unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Regions
Northwest Inland.
Confidence
Fair - Due to limited field observations
Weather Forecast
Monday: Up to 10cm of new snow - moderate to strong easterly winds - freezing level at surface Tuesday: Light snowfall - light to moderate southwesterly winds - freezing level at surface Wednesday: Light snowfall - moderate southeast winds - freezing level rising to 600m
Avalanche Summary
No new avalanches to report. We'd love to hear about what you've seen in the field. Any observations can be sent to: [email protected].
Snowpack Summary
Warm temperatures and then subsequent cooling have created crusts on all aspects below 1000m and on sun-exposed slopes as high as 1600m. More recently, intense wind-loading and light snowfall accumulations have taken place with snow surfaces either getting scoured or packed into hard wind slabs. The mid February interface, down around 60cm, is variable and generally consists of a strong melt freeze crust below 1000m. Above that elevation, expect to find buried facets, and/or surface hoar (in more sheltered areas), and/or a sun crust on southern aspects. The surface hoar is not widespread, but has been responsible for larger avalanches that occurred last week. This layer should be on your radar, as it may be susceptible to rider triggers.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.
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.