Avalanche Forecast

Issued: Feb 26th, 2015 10:00AM

The alpine rating is moderate, the treeline rating is moderate, and the below treeline rating is low. Known problems include Wind Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Shallow new wind slabs potentially formed on westerly aspects may be found near and above treeline Friday.  

Summary

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 loading westerly aspects mainly near and above treeline.  

Currently there is not enough new snow forecast to increase the avalanche risk at below treeline or in wind sheltered areas. 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 mild 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 especially further from the crest.

A few weak weather disturbances passed through under NW flow aloft last week, bringing an inch or two of new snow near and above treeline and near the Cascade crest. Winds veered to the east or northeast on Saturday, causing shallow new wind slab formation on non-traditional westerly to more southerly aspects primarily above treeline.  

Observations in the Rainy Pass area over the weekend noted shallow wind slabs of 15-25 cm (6-10 inch) forming on SE-S-SW facing slopes, with cracking but no releases observed. With mild daytime temperatures earlier this week, these isolated slabs have likely further stabilized. 

Significant surface hoar growth was observed in the Washington Pass area Wednesday, even on solar aspects. We'll see if we receive any new snow for this to become a future problem. 

While the January 15th facet/crust layers can still be identified in parts of the NE Cascades, this persistent weak layer has been stabilizing and become unlikely to trigger. As a result the Persistent Slab problem has been removed from the northeast zone.

Problems

Wind Slabs

An icon showing Wind Slabs

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.

 

Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..

 

Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.

 

Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.

Aspects: South, South West, West, North West.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Feb 27th, 2015 10:00AM