Avalanche Forecast

Archived

Mar 7th, 2016–Mar 8th, 2016

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural and human triggered avalanches likely.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches possible, human triggered probable.

Regions

Olympics.

You will need to watch for new layers in some areas and for a combination of winter and spring conditions if you venture out on Tuesday.

Detailed Forecast

A weakening front should move over a flat ridge and over the Northwest Tuesday afternoon and night. Snow from this front should mainly reach the Olympics, the southwest Cascades and at Mt Hood by the end of the daylight hours on Tuesday.

New snow may be enough to form new wind and storm slab layers mainly in the above tree line zones in the Olympics, the southwest Cascades and at Mt Hood by the end of the daylight hours on Tuesday. A rule of thumb is that storm slab is likely when snowfall accumulates at more than an inch an hour for several hours.

Older or previous wind slab may also still be present near and above treeline. Watch for firmer wind transported snow.

Loose wet avalanche conditions may still be possible mainly on solar slopes below tree line along the west slopes. Watch for wet snow deeper than a few inches, pinwheels and natural loose wet avalanches.

Snowpack Discussion

Weather and Snowpack

Last week was wet and relatively mild with a series of active fronts transiting the region resulting in fluctuating freezing levels and periods of very strong winds. The heaviest snowfall and precipitation occurred late Sunday 2/28 and Tuesday 3/1.

The mid and lower snow pack in the Olympics should generally be a stable mix of crusts and layers of moist and rounded snow crystals.

Recent Observations

The ranger at Hurricane reported a foot of new snow on Monday morning with snow sliding off the road cuts and onto the road in many places. The Sunrise path on a northeast slope about a 1/2 mile from the visitor center released an avalanche that entrained to about 1' and became 100 feet wide although it could not be determined if it was a loose or slab avalanches due to low visibility.

Problems

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). 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.

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.