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RegisterDec 24th, 2017–Dec 25th, 2017
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Recent wind slab and storm snow should continue to stabilize. Avoid steeper terrain features with firmer wind transported snow. Be prepared to ratchet back from your plans if there is more snow than expected Sunday night.
A weakening front and a weak surface low will move across the Northwest Sunday night. The main snow should be seen in the south Cascades and mainly at Mt Hood. Light amounts of new snow if any are expected along the Cascade east slopes. Watch for a change Monday to light to moderate W-NW alpine winds. Temperature fluctuations could be a little problematic.
So not a lot of change is expected on Monday. This should mainly continue to allow recent storm snow to gradually stabilize.
Keep an eye out for previous or newly forming wind slabs on Monday. Winds will have potentially load non-traditional aspects. If you see signs of winds transporting snow including plumes, drifts, and uneven snow surfaces, then avoid slopes where the wind loading is occurring.
Also despite all this new snow, early season hazards still exist at lower elevations and especially around creek beds that are not filled in.
Lots of uncertainty exists around the distribution and sensitivity of the 12/15 layer. Limited observations on this layer make it difficult to forecast. When uncertainty goes up, terrain selection must go down to maintain wide margins of safety. Time and patience will allow this layer to gain strength.
A few inches of light snow fell across the east slopes of the Washington Cascades in the 24 hours ending Saturday morning. Up to about 3 feet of recent snow sits atop the 12/15 crust/persistent weak layer. Overall recent snow has been gaining strength leading to a recent stabilizing trend.
Ridge top winds Tuesday to Thursday and possibly again Sunday redistributed snow in exposed and wind prone areas forming wind slabs on a variety of aspects.
A large amount of uncertainty exists around the 12/15 crust/persistent weak layer. This layer has generally been observed at elevations below 6000 feet. Snowpack tests in a few locations continue to demonstrate results and the potential for an avalanche to propagate. The limited amount of incoming information makes it difficult to paint a clear picture of this potential avalanche problem.
A rain crust, a few inches above the 12/15 crust, is seen in some pits in some areas below treeline east of the crest.
Snowdepth decreases substantially the further east from the Cascade crest. In many areas below treeline, there is not enough snow to present an avalanche danger.
Observations
North
Many observations are coming via the NCMG for the Washington Pass corridor through the week.
On Saturday in the Washington Pass Hairpin area on southwest slopes 5500-7200 feet recent snow was well bonded and small steep slopes did not give results in slope tests. There was widespread new surface hoar.
On Friday at the Washington Pass Hairpin they found 45-65 cm of storm snow on the 12/15 crust, with an ECTP21 result in 2 cm buried surface hoar on the 12/15 crust. However, the buried surface hoar was not seen in pits above 5300 feet.
On Thursday on Delancey Ridge they noted blowing snow, moderate CT results in storm snow and a ECTP result between crust layers at about 48 cm.
Central
On Thursday, professionals on Dirtyface Peak observed the 12/15 layer/PWL interface reactive in PST and ECT tests at 5000 ft on an east aspect. The interface was 2.5 ft down. Wind transport was occurring near and above treeline and actively loading lee slopes. Recent storm instabilities were healing.
South
No recent observations