Avalanche Forecast
Regions: Cascades - East.
Recent new snow and winds have covered a pronounced weak layer, creating a recipe for dangerous avalanches conditions. Safe travel through avalanche terrain will require a very cautious approach and conservative decision making.
Discussion
The first 9 days in December were clear and cold. Surface hoar grew large during this time, and facets developed near the surface of the cold, low density snow. On December 9th this layer was covered up and preserved on many aspects and elevations. A widespread natural avalanche cycle was documented in adjacent regions on December 11th. A professional observer reported a large natural avalanche in the Spire Gully on Washington Pass with an impressive powder cloud. Near here, the observer reported triggering avalanches remotely (from a distance) and had widespread collapses on the old snow layer. Test results indicated the potential for wide propagation on this layer of buried surface hoar and near surface facets. On December 12 an observer reported shooting cracks up to 20 feet long at Mission Ridge. Due to the nature of the geography, there is a large range in snowpack depths from West to East in this zone. This means that there is likely a wide range in slab thickness associated with the December 9th weak layer, but it is likely to be found from one to three feet deep.
Observations from East Central Forecast Zone have been very limited, as it is early season and not many folks have been up yet. Please share your observations if getting out, thanks!
Snowpack Discussion
Regional Synopsis 20181213
Winter is here.
A productive winter storm pattern has elevated the avalanche danger and provided an interesting start to the season. Â
A quick breakdown:
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Tuesday and Wednesday saw a significant localized avalanche cycles.
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We have a lot of new snow...2â to 5â above 4500ft.
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Weâve gotten a lot of wind.
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We have weak layers near the ground.
Dangerous avalanche conditions will persist over the next couple of days. That said, it is early season and the flavor of avalanche you may run into is likely a function of elevation, timing, and dumb luck.
Here are some basic emerging patterns:
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Snowfall totals so far this week (Monday morning to Thursday evening) illustrate more recent snowfall in the north than the south:
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Mt. Baker: 55â
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Washington Pass: 29â
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Stevens Pass: 37â
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Snoqualmie Pass: 28â
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Paradise: 38â
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Mt. Hood Meadows: 13â
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Upper versus Lower Elevations: The change in the snowpack is still pretty dramatic with elevation. Height of snow decreases rapidly below 4500â at Baker and Washington Pass, 5500â at Crystal/Rainier. The Passes have better low elevation coverage, but it's still pretty thin below 4000â. With additional warm storms in the forecast, this pattern is expected to continue for awhile.
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East versus West: Loading along the East slope has been more incremental, and a  variety of buried facet and surface hoar layers may be found. This is most pronounced near WA Pass. Although significant snowfalls and precip totals have resulted in thicker, more homogeneous snowpack in the western zones, lingering weak layers near the ground will persist through the week.
The uncertainty of how reactive our buried weak layers are will carry into the weekend. Be cautious and get home safe.
Avalanche Problems
Persistent Slabs
Slabs from one to three feet thick are sitting on old, weak snow. The telltale signs of instability with this layer are whumphing and collapsing. These signs may or may not present itself, but any failure on this deep, weak layer would be surprising and scary. It is recommended to respect avalanche terrain and dig down to look for this layer. Enter avalanche terrain with respect, as safe travel through it will require a very cautious approach.
Release of a cohesive layer of soft to hard 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 Slabs.
The best ways to manage the risk from Persistent Slabs is to make conservative terrain choices. They can be triggered by light loads and weeks after the last storm. The slabs often propagate in surprising and unpredictable ways. This makes this problem difficult to predict and manage and requires a wide safety buffer to handle the uncertainty.
This Persistent Slab was triggered remotely, failed on a layer of faceted snow in the middle of the snowpack, and crossed several terrain features.
Persistent slabs can be triggered by light loads and weeks after the last storm. You can trigger them remotely and they often propagate across and beyond terrain features that would otherwise confine wind and storm slabs. Give yourself a wide safety buffer to handle the uncertainty.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Likely
Expected Size: 1 - 1