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Avalanche Forecast

Archived

Mar 19th, 2016–Mar 20th, 2016

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

Olympics.

A mixture of typical spring avalanche problems exists with no one problem dominating. Evaluate the local snow and terrain carefully on Sunday.

Detailed Forecast

Cloudy Sunday with periods of mostly light rain or snow showers and mild conditions are expected. Rain and snow amounts should be relatively light and not significantly affect the current danger.

Temperatures should remain above freezing Saturday night and with the addition of light rain near and below treeline, small loose wet avalanches may be possible on Sunday. Loose wet avalanches may start small but could have the ability to entrain recent moist snow in mainly on steep terrain.

Strong winds near ridgetop may combine with light precipitation to build new areas of wind slab on lee aspects in the upper elevations above treeline. Any new wind slabs will mostly likely be found in NW-NE facing slopes. Firm wind transported snow and snowpack cracking can be good signs of wind slab layers.

Recently formed cornices have grown large and can become sensitive during mild weather, especially following nights with above freezing temperatures.  Avoid areas on ridges or summits where there may be a cornice and avoid slopes below cornices in the spring.

Snowpack Discussion

Weather and Snowpack

A combination of sun and mild temperatures over the past three days have allowed for the 2-3 feet of storm snow received since March 10th to settle and stabilize while forming a strengthening surface crust on most slopes. 

Periods of strong to very strong winds during storm cycles likely created wind and storm slab layers in the Olympics, though these layers have likely settled and stabilized over the past several days of mild weather. 

These recent storms have also built large cornices along ridges with some recent releases.

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

Recent Observations

A Hurricane Ridge Park ranger found variable surface crusts Saturday morning, as overnight temperatures remained well over freezing.   

While over a week old now, NWAC pro-observer, Matt Schonwald toured around the Hurricane Ridge area Friday 3/11. He found up to 20 cm of dense 1 F or P snow above the latest rain crust. Thin wind slabs were generally not reactive except in isolated areas on N-NW lee aspects near treeline. Although cornices were large, they were generally firm and not sensitive. Windward slopes that had melted out a few weeks earlier had firm, and in places, icy thin coverage. Overall Matt noted few current avalanche problems in the Hurricane Ridge area Friday, March 11th.

The Hurricane ranger did not see evidence of loose wet avalanches along the road on the drive up on Friday morning 3/18.

Hurricane Weather Station

Internet communications to the station have been disrupted at the NWAC office. We have a repair on-going with a technician and are hoping to be back online shortly.  We apologize for the outage and thank you for your patience.

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.