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Avalanche Forecast

Archived

Mar 19th, 2017–Mar 20th, 2017

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

Regions

Stevens Pass.

The avalanche danger should decrease further on Monday. E-SE winds may distribute shallow amounts of recent snow onto westerly aspects near and above treeline. Increasing clouds should lower the likelihood of small loose wet slides. 

Detailed Forecast

Increasing cloud cover should quickly spread from south to north over the Cascades on Monday. Precipitation may develop for the southern Washington Cascades Monday afternoon but hold off until the evening for areas further north. Offshore gradients will create locally breezy east winds near the Cascade Passes.  

The avalanche danger should decrease further on Monday. Light to locally moderate E-SE winds may distribute shallow amounts of recent snow onto westerly aspects near and above treeline in the central Cascades. In the southwest Cascades, recent or fresh wind slab will more likely be found above treeline. Older wind slab may linger on NW to SE aspects. Watch for firmer wind transported snow on all aspects, especially in areas of complex terrain. 

Increasing clouds should lower the likelihood of small loose wet slides Monday. If solar radiation is more intense than forecast, expect the likelihood for natural and human triggered loose wet avalanches to increase on steeper solar slopes. Watch for surface wet snow deeper than a few inches, rollerballs or increasing small natural releases. Avoid areas with terrain traps where a small loose wet avalanche could have unintended consequences. 

It is always a good plan to travel well back from ridges, suspected of cornice formation, or on steep slopes below cornices.

Snowpack Discussion

Weather and Snowpack 

The first week or so of March was very cool and snowy. NWAC stations along the west slopes of the Cascades piled up about 3 to 8 ft of snow with the most at Mt Baker.

The 2nd week of March was equally active with non-stop Pacific frontal systems pummeling the PNW. Unfortunately these systems delivered far more rain than snow. At least two regional avalanche cycles occurred during the stretch. Significant snowpack consolidation occurred over this period due to rainfall and warmer temperatures. 

After a short respite from the active weather pattern on Thursday, another strong low pressure system brought several inches of rain to the west slopes of the Cascades outside the Cascade Passes Friday night. 2.5 to 4 inches of water was seen at Paradise, Crystal and Mt. Baker respectively over the 24 hours ending at 5 PM PDT Saturday, mainly in the form of rain. Stevens and Snoqualmie Pass picked up 6-8 inches of new snow Friday night before changing to rain later Saturday morning.

Rapid cooling with the frontal passage produced about 8 inches of snow at Mt. Baker with lesser amounts seen elsewhere along the west slopes of the Cascades late Saturday morning through Saturday evening. Sunday was cool with light winds with a general clearing trend seen throughout the Cascades.  

Recent Observations

North

Early Saturday morning, Mt. Baker pro-patrol reported widespread natural loose wet activity that had occurred Friday night off of Table Mt, Mt. Herman and Shuskan Arm. Very heavy rain overnight had increased the potential for wet slab/glide avalanches in the Mt. Baker area. 

NWAC observer Lee Lazarra was in the Ptarimgan Ridge area of the Mt Baker backcountry Sunday.  There was widespread evidence of the most recent wet snow avalanche cycle from Friday night with debris at the bottom of many avalanche paths. Crowns from wet slabs were especially large below treeline. Lee found the most recent rain crust very supportable above treeline but still in the process of re-freezing below 4500 feet. Small loose wet slides released naturally and ran well on steeper solar slopes during clearing in the afternoon.  About 20 cm (8") of recent storm snow was evenly distributed regardless of elevation. Isolated pockets of shallow wind slab were found above treeline but no obvious loading pattern was discernable. 

Central

Alpental pro-patrol reported easy and widespread ski triggered 6-8" storm slabs on the upper half of Alpental Saturday morning with rain reaching the summit. Loose wet avalanches were easily triggered later in the day on steeper slopes. Stevens Pass pro-patrol had similar results Saturday morning with widespread sensitive loose wet slides, up to size 2, natural and human triggered during the warming and switch to rain.  

South

Crystal patrol reported a natural cycle Friday night, presumably loose wet, but little to no results during avalanche control work Saturday morning.  On Sunday, Crystal pro-patrol reported a stout rain crust on the upper mountain with about 5-8 cm (2-3 in.) of well bonded snow on top of the crust. 

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.

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.