Avalanche Forecast
Issued: Jan 4th, 2018 10:14AM
The alpine rating is Wind Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeLight snow and wind above treeline may develop small wind slabs during the daylight hours. Monitor changing snow surface conditions throughout the day and be prepared to change your travel based on current conditions.
Summary
Detailed Forecast
Light precipitation in the form of rain will continue to break down surface crust causing them to become less supportable at near and below treeline. Loose wet avalanche may occur but would be limited to very isolated terrain where surface snow becomes sufficiently wet to lose cohesion. Loose wet activity is expected to peak during Thursday night and diminish rapidly into Friday.
Above treeline, snow combined with southerly winds will develop small wind slabs on lee slopes during the day. Expect this avalanche problem to continue to grow throughout the day as more snow becomes available for transport by the wind.
Despite all this new snow, early season hazards still exist. Many creek beds have still not filled in for the winter.
Snowpack Discussion
Light rain Thursday began to soften surface crusts on most slopes.
A variety of snow surfaces exist, including wind scoured snow, crusts, and likely stubborn to unreactive wind slabs.
Several rain and freezing rain crusts are sandwiched in the upper snowpack depending on elevation. Current observations do not suggest these layers to be reactive.
Observations
Mt Hood Meadows Ski Patrol reported a melt-freeze crust at the surface Thursday prior to the precipitation event.
Problems
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: North, North East, East, West, North West.
Elevations: Alpine.
Likelihood
Expected Size
Valid until: Jan 5th, 2018 10:14AM