Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Apr 27th, 2017–Apr 28th, 2017

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

.

Increasing spring sun can quickly melt night time surface crusts and rapidly activate loose wet snow and result in a dramatic increase in avalanche danger. Continue to give potential cornices a wide berth if traveling along ridge-lines and avoid slopes below cornices. A good way to manage spring time risk is to start early and be out of avalanche terrain by afternoon.

Detailed Forecast

Fair weather with a modest rise in cool temperatures and low snow levels should be seen on Friday.

Loose wet avalanches are possible on solar slopes. Increasing spring sun can quickly melt night time surface crusts and rapidly activate loose wet snow and result in a dramatic increase in avalanche danger. Watch for surface wet snow deeper than a few inches, pinwheels and initial small loose wet avalanches that indicate an increasing loose wet avalanche danger.

Small wind slab will be possible above treeline on lee aspects. NWAC stations along the Cascade crest have had moderate to very strong west winds on Wednesday and Thursday. So this is most likely on NW to SE aspects but watch for firmer wind transported snow that is a sign of wind slab on other aspects in areas of varied terrain.

Cornices are still large so give them a wide safety margin. Natural cornice releases and resulting slab avalanches are dangerous and unpredictable. Give potential cornices a wide berth if traveling along ridge-lines and avoid slopes below cornices. See a blog post regarding cornices here.

Avoid unsupported slopes with overhanging blocks of snow and smooth rock underneath. Glide avalanches are difficult to predict and can release at any time, not just during the heat of the day.

 

Snowpack Discussion

A cool, snowy pattern has been seen in late April for the mainly for the Cascade west slopes and especially for the Mt Hood area.

Last week from Monday 4/17 to Thursday 4/20 NWAC weather stations along the Cascade east slopes picked up about half an inch of water equivalent (WE). Much of this modest amount of WE fell as snow above 5500-6000 feet.

A fair day was seen last Friday with most NWAC stations in the Olympics and Cascades reaching the 40's and 50's.

The current storm cycle began on Saturday. For the 5 days ending Thursday morning NWAC stations along the Cascade east slopes had modest amounts of WE and light snowfall.

Recent observations

The Washington Pass DOT crew on Thursday reported no significant, recent avalanche activity.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

Wind Slabs

Wind Slab avalanches are the 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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.