Avalanche Forecast

Issued: Jan 15th, 2018 11:03AM

The alpine rating is moderate, the treeline rating is low, and the below treeline rating is low. Known problems include Wind Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Lowering snow levels and winds on Tuesday will develop shallow wind slabs above treeline. Mitigate hazard by approaching lee slopes with caution and observing new snow amounts and snow transport, which may extend into the near treeline zone in areas that see more snowfall than anticipated.

Summary

Detailed Forecast

A weakening cold front should bring a brief period of light rain and snow Monday night, with the rain/snow line into the above treeline terrain. Further cooling should follow the front and rain/snow showers will re-develop behind the front during the day Tuesday and light to moderate SW crest-level winds will transport the new snow as it accumulates. The old snow surfaces are expected to begin to refreeze at higher elevations as temperatures cool. New snowfall on Tuesday is anticipated to bond well to the refreezing snow surfaces.

Watch for the development of shallow wind slabs, particularly on NW through SE aspects above treeline. Monitor new snow and wind transport diligently throughout the day and avoid wind-loaded slopes.

Note that a variety of snow conditions may be encountered on Tuesday, including breakable crusts, wet snow, new snow over refreezing surfaces, etc.

Snowpack Discussion

Inversion conditions since the last storm have enabled the initially dry snow at higher elevations to undergo 3 days of melt-free cycles, forming crusts of variable thickness on most aspects at night and wet snow surfaces during the day. At lower elevations, snow was previously saturated, but here temperatures have remained near or slightly above freezing within the inversion layer.

Surface hoar up to 1 cm has been observed in some locations, such as Blewett Pass, on non-solar slopes during this period.

Last week’s storms brought 8-14 inches of snow to the east slopes of the Cascades. Winds throughout the storm period redistributed snow, forming wind slabs on a variety of aspects especially in exposed terrain that continue to strengthen over the past several days.

A supportive crust (1/5) formed from a widespread freezing rain event in the central-east zone, extending to the Stevens and Snoqualmie Pass areas. This layer is not present in the northeast from Washington Pass to Holden.

Snowdepth still decreases substantially east of the Cascade crest. In many areas below treeline, there has not been enough snow to present an avalanche danger.

Observations

North

North Cascades Heli was in the field Saturday and observed thin wind slabs, 8 inches thick on lee slopes. Roller balls were reported on sunny slopes in the afternoon, but natural loose wet avalanche was not observed.

Guides from both North Cascades Mountain Guides and North Cascades Heli were in the field Friday. Observations suggest storm snow weaknesses are gaining strength.

Central

Mission Ridge Pro Patrol Friday reported upside-down new storm snow. Avalanches observed failed within the storm snow.

Older but still relevant observations:

Several observations from the Mission Ridge and Blewett Pass areas have reported 2-3mm facets on the ground, including a recent post found here. Another report near Mission ridge found a facet layer 45 cm above the ground. These layers will need to be monitored as they could develop into potentially dangerous weak layers in the future.

South

No recent observations

Problems

Wind Slabs

An icon showing Wind Slabs

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.

 

Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..

 

Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.

 

Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.

Aspects: All aspects.

Elevations: Alpine.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Jan 16th, 2018 11:03AM