Avalanche Forecast
Regions: Cascades - South East.
Watch for recently and newly forming storm and wind slabs, especially on wind loaded slopes near ridges and if venturing to higher elevations. Watch for early season terrain hazards, such as poorly covered rocks, vegetation and creeks, particularly at lower elevations.
Detailed Forecast
A weak to moderate front should move across the Cascades near midday Thursday, causing a period of light to briefly moderate snow and moderate ridge level winds. This weather should build new areas of storm and wind slabs, especially in wind affected terrain, such as higher elevations and near ridges.
Watch for storm slabs in areas that received more than a few hours of moderate or heavy snowfall intensities.Â
Watch for firmer wind-transported snow on lee slopes near ridges, generally northwest through southeast aspects, but expect wind deposited snow on a variety of aspects in areas of more complex terrain.
Storm or wind slab avalanches may entrain recent snow down to the firmer old refreezing snow from last week.
Although not  listed as a current avalanche problem, loose dry avalanches are possible Thursday, particularly on steep slopes.Â
Watch for the numerous travel hazards such as open creeks, barely buried rocks and trees, creating poor and challenging travel conditions, especially below treeline.Â
The avalanche danger should generally increase for all elevation bands on Thursday.
Snowpack Discussion
The great start to the 2017/18 PNW Winter hit the pause button last week throughout the Cascades during an extended period of warm and wet weather. Several cycles of wet snow and glide avalanches occurred, especially on steep unsupported slopes and rock faces.Â
Over the weekend, the weather system that brought rain to the rest of the Cascades brought several inches of snow Saturday night through Sunday at Washington Pass. Mixed precipitation or a brief period of rain may have occurred Sunday afternoon as temperatures warmed aloft. Â
Little to no new snowfall was seen for most of the central-east and southeast Cascades over the weekend due to warmer temperatures and a period of rain. Snow depths are limited in these areas.
On Tuesday, a frontal passage brought a slight bump in snow levels into the 3000 ft range and deposited about 5-10 inches or more of new snow as of Wednesday morning. The greatest recent storm totals were received in the northeast Cascades.
Observations
On Tuesday in the Slate Creek drainage in the northeast zone, between about 5400-7250 feet, NWAC observer found about 1-2 feet of low density snow bonding well to a thin crust from last week. The new storm snow was not slab like in the areas travelled and no avalanches were triggered or observed. There was potential for wind slabs in specific terrain above treeline, but no avalanches were directly observed.  Â
Avalanche Problems
Storm Slabs
Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. 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.
You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.
Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1
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, South East, North West.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1