Lawinenlagebericht

Stevens Pass

Feb 26 – 27, 2015Northwest Avalanche Center
Auf der Karte ansehen
Archiviert · abgelaufen 12 years ago

Lawinengefahr

Sat
Hochgebirge
2 · Mässig
Waldgrenze
1 · Gering
Unterhalb
1 · Gering

Kernpunkte

Shallow new wind slabs potentially formed on a variety of aspects may be found above treeline Friday.  

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1

Detailed Forecast

Generally light snowfall amounts are expected Thursday night and Friday.  However, winds should increase and back to SE Friday morning and then to ENE Friday afternoon, potentially creating shallow new wind slab and cross-loading slopes mainly above treeline.  

Currently there is not enough new snow forecast to increase the avalanche risk at lower elevations. If the forecast goes awry, make sure to change your travel plans accordingly. 

Due to the low snowpack, especially below treeline, watch for terrain hazards such as open creeks, partially covered rocks and vegetation. Many areas below treeline do not have enough snow (new or existing) to pose an avalanche hazard. 

Snowpack Discussion

Since the warm and wet start to February, fair weather through mid-February has led to generally thick surface crusts, as well as further deterioration of the snow cover below treeline. 

A few weather disturbances passed through a week ago, bringing a welcome few inches of snow near and above treeline. Winds veered to the east or northeast last Saturday, causing some new wind slab formation on non-traditional more westerly to southerly aspects mainly above treeline. A few reports of ski-triggered shallow wind slabs were reported from the west slopes over the weekend, generally found above treeline.  

Generally 1 to 3 inches of snow accumulated at NWAC sites Wednesday night through Thursday afternoon above about 4000 ft with rising snow levels in the afternoon. No significant avalanche problems were expected or reported.   

The mid and lower snowpack west of the crest snow consists of layers of stable consolidated rounded grains or melt forms and crusts from multiple warm periods this winter.

 

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