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Avalanche Forecast

Archived

Dec 15th, 2015–Dec 16th, 2015

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

Regions

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Previous wind and storm slab layers from the weekend should be the main concerns on Wednesday. Greater caution would be necessary if the weak front Tuesday night and Wednesday morning brings more snow than expected.

Detailed Forecast

A weak cold front will cross the Northwest Tuesday night and Wednesday morning. This may bring some very light amounts of new snow but should not greatly change conditions. Some fair weather should be seen by Wednesday afternoon. Light or moderate northwest winds and cool temperatures should also continue on Wednesday.

Previous wind slab layers from the weekend will possibly linger on previous lee mainly north to east slopes near ridges and summits on Wednesday. Storm slab from the weekend should become unlikely by Wednesday but would be found in what were calmer areas if it still exists.

Use more caution and watch for new small wind slab or small storm slab if the weak front Tuesday night and Wednesday morning brings more snow than expected. This is mainly possible in the Snoqualmie Pass area.

Terrain anchors are still causing significant anchoring at the lowest elevations. Use caution near creeks which are still open in some areas.

Snowpack Discussion

An atmospheric river caused warm very wet weather last week. About 5-8.5 inches of rain was seen along the west slopes. This caused an avalanche cycle, consolidation and stabilizing of the older part of the snowpack along the west slopes and is expected to have eliminated persistent weak layers at Stevens and Snoqualmie.

A stormy pattern with cooling was seen late last week and over the weekend with about 1.5-4 feet of snowfall along the west slopes.

Reports varied on Sunday. The Mt Baker and Alpental pro patrols reported widespread avalanches released from explosives ranging from 1-2 feet and running good distances, releasing on storm snow interfaces. The Stevens Pass pro patrol reported morning control produced widespread soft slab results from both explosive and ski cuts with best results on NW-SE facing terrain with slides releasing on the most recent storm interface with Friday's storm snow. Across the street at Skyline Ridge at Stevens Pass NWAC pro observers found about 30-60 cm of mostly stable, mostly right side up storm snow, well bonded to Tuesday's rain crust. One 30-40 cm storm slab was triggered on a 40 degree slope which ran on the crust from early last week.

Cool weather with little new snow has been seen Monday and Tuesday. This will have mostly caused some consolidation and further stabilizing.

We do have one more report via the NWAC Observations page of a 25 cm slab that was triggered on a steep north-northeast facing slope at Stevens Pass on Monday. The NWAC pro observers had a field training Monday and Tuesday at Stevens Pass and found a graupel or stellar layer at 35-40 cm but tests did not indicate propagation. Rain from last week had percolated well down into the snowpack.

 

 

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.