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Avalanche Forecast

Archived

Dec 27th, 2015–Dec 28th, 2015

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Olympics.

Storm and wind slabs may be sensitive to human triggering Monday. Remember MODERATE danger means human triggered avalanches are possible. Recent unconsolidated storm snow is still very deep in places with possible large tree wells lurking, so stick near your partner in the trees. 

Detailed Forecast

Wind slab will most likely be found on north to southeast aspects near and above tree line. NW winds will redistribute new snowfall to lee SE slopes near and above treeline Monday. Wind and storm slab avalanches should stay within recent storm layers. Test for inverted strong over weak storm snow and give recently formed cornices a wide margin.

Beware of loose dry avalanches in steep non-wind affected terrain that could have unintended consequences such as knocking you off your feet and into a terrain trap.

There have been snow immersion fatalities in tree wells already this season at Snoqualmie and in Canada. Recent unconsolidated storm snow is still very deep in places with possible large tree wells lurking, so stick near your partner in the trees and maintain visual contact.  

Snowpack Discussion

We have had about a week of heavy snow and cool temperatures in the Olympics and Cascades. The Hurricane Ridge NPS Ranger reported a snowdepth of 87 inches Sunday morning with about 4 feet of new storm snow since the 21st. There has been slow settlement over the last few days, but the main message is that it is still deep out there!

In non-wind affected areas, the upper snowpack should generally be right side up with increasing hardness with depth. Unlike last year, there is a healthy snowpack below treeline on all aspects. A NPS Ranger also reported a widespread natural avalanche cycle had occurred within the last few days within the Hurricane Ridge area, with extensive storm slab activity seen on a variety of aspects near and below treeline. A few more inches of new snowfall along with moderate southerly transport winds on Sunday loaded lee slopes well below ridge-lines. NWAC observer Matt Schonwald found a skier triggered 1'-3' soft wind slab release on a north slope that easily propagated 150'. He did not find sensitive wind slabs throughout the terrain, even on similar aspects and elevations.  Matt also reported that corncies were quite large and posed their own hazard due to their size.   

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.

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.