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Avalanche Forecast

Archived

Mar 4th, 2017–Mar 5th, 2017

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

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Very large natural and triggered avalanches are being reported Saturday. Avalanches in this zone should be large to very large and backcountry travel is not recommended Saturday.

Detailed Forecast

Decreasing winds and mostly light to moderate snow showers should be seen over the Cascade west slopes on Saturday with much lower snow levels and much cooler temperatures. 

Large unstable storm and wind slabs should persist Saturday. Natural or triggered avalanches will remain likely to very likely. Avalanches should be large to very large.

Very dangerous avalanche conditions.

Travel in avalanche terrain is not recommended. 

Snowpack Discussion

Weather and Snowpack 

...Updated 115 PM. Mt Baker area received over 2 feet of new snow as of Saturday morning. Reports of natural and human triggered large avalanches, many 3-5 foot crowns! In the Mt Baker backcountry, Mt Herman, 4-5' triggered slide released nearly 1/4 wide, including a partial burial.

The most recent wet warm storm arrived on Valentines Day 2/14 and formed the uppermost, very strong rain crust in the snowpack. 

A series of disturbances in cool, NW flow aloft from Saturday 2/25 through Tuesday 2/28 deposited 1.5 - 3.5 feet of snow along the west slopes of the Cascades. Very strong alpine west winds were seen in most of the Olympics and Cascades on Tuesday.

Southwest flow aloft began to ramp up again on Thursday as the first in a new series of fronts crossed the Northwest. Strong southwest flow is carrying a second stronger front across the Northwest on Friday evening. Along the Cascade west slopes this will be causing strong southwest alpine winds, heavy, moist, dense new snow above about 3-4000 ft and wet snow or rain below about 3-4000 ft. An avalanche cycle is expected in many areas along the Cascade west slopes Friday afternoon and evening.

Recent Observations

North

Updated 115 PM Saturday - Widespread natural and triggered large avalanches, many 3-5 feet crowns with wide propagation on Shuksan Arm. Partial burial reported from triggering a slide on Mt Herman, a crown of 4-5 feet by 1/4 mile wide! Fortunate outcome.  

NWAC observer Lee Lazzara reported that extensive avalanche control was needed at the Mt Baker ski area on Friday but further detail are not currently available. Lee found an upside down warmer, wetter over drier, weaker profile and that test columns were failing on isolation in storm snow layers. A general top of the snowpack profile was 30-40 cm of 1F+ over 4F snow.

Central

NWAC observer Jeremy Allyn was in the Alpental Valley on Thursday and found storm snow instabilities still present and slowly stabilizing. Thin wind slab was forming in the upper portion of the below treeline band and showed signs of increasing sensitivity.

The Stevens patrol reported widespread 6-8" ski triggered storm slab on Friday morning. Sensitive loose wet ski tests were also seen below about 4500 ft.

NWAC observer was also at the Stevens ski area on a day off from the NWAC but reported upside down wetter over drier snow conditions.

Extensive 4-14" wind slab triggered by explosive control turned into wet debris at Alpental on Friday morning.

South

No recent observations.

Problems

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.

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.