Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 18th, 2017–Jan 19th, 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 unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

.

A drastic change from the recent weather is underway. Warmer snowy weather should substantially increase the avalanche danger through Wednesday. Natural wet snow avalanches are likely and travel in avalanche terrain is not recommended.  

Detailed Forecast

An avalanche warning is in effect through Wednesday afternoon.

Along the east slopes expect strong winds and snow with warmer temperatures through Wednesday afternoon. The warmer temperatures will potentially allow denser heavier wind or storm slab to further build over lower density snow layers.This will further build potentially deep new wind and storm slab along the east slopes.

An abundance of weak and cold snow in the upper snowpack especially near and below treeline combined with further warming and high precipitation rates should lead to very dangerous avalanche conditions during this period along the east slopes and backcountry travel is not recommended. 

The 12/17 PWL and other persistent weak layers closer to the surface have been unreactive as of late. If this layers does not snow reactivity during the current storm cycle it will be removed as an avalanche problem.

Snowpack Discussion

Weather and Snowpack

A pair of warm fronts moved across the Northwest last weekend, which allowed some relatively milder Pacific air to finally work its way east of the crest Sunday evening and night. 3-8 inches of snow fell through Monday morning, 1/9 along the east slopes. 

A weak low pressure system, tracking across Oregon Tuesday morning through Wednesday afternoon produced 1-5 inches of snow in the central east to southeast Cascades with the most seen at the Lost Horse and Potato Hill Snotels in the southeast Cascade zone. E to NE winds increased Tuesday afternoon.

Snow showers deposited another 2-4 inches early Wednesday in the southeast Cascades zone, with little or no snow in the north and central.

An upper ridge over the northeast Pacific Ocean has caused fair weather Thursday through Sunday over the Cascades with mostly light winds and moderating temperatures seen mainly at higher elevations along the east slopes due to strong temperature inversions. Low clouds over Eastern Washington stayed banked up against the east slopes over the weekend while the mountains mostly enjoyed the sunshine. 

Surface hoar and near surface faceting has been noted widely throughout the range in sun and wind sheltered locations below treeline. Sun crusts have formed on steeper solar aspects over the last few days.

Many small loose-wet slides were seen on solar aspects at higher elevations during the mild, mostly sunny weather Monday, MLK Holiday. 

Warm, wet and windy weather has returned to the Cascades as Tuesday with the rain intensities increasing Tuesday afternoon, 1/17 to all elevation bands. 

Recent Observations

NWAC pro-observer Tom Curtis was on Mt Cashmere Wednesday and pulled the plug on continuing a tour due to the conditions observed. The sound of a natural avalanche rang out loudly in the valley Wednesday morning. It was estimated the slide released from a more westerly aspect near tree line. Other concerning observations included finding a reactive buried thin crust with faceted crystals below and a 25-35 cm 4F slab above. Cracks were shooting from skis and snowpit tests also indicated human triggered slab releases would be likely in this area.

The NCMG were at Washington Pass on Wednesday and reported that wind slab from last weekend was primarily seen on E-SE terrain features and was becoming less reactive.

A couple reports via the NWAC Observations page are available for Wednesday. A report from Mt Cashmere indicated a shallow, variable snowpack with evidence of wind loading from last week. A collapse and snowpack cracking was seen on a southeast slope at 5300 feet due to a facet/crust layer at 35 cm down but these layers were not found to be widespread. A skier also reported 14-16 inches of snow and snowpack collapsing on Manastash Ridge on Wednesday.

Tom Curtis was on Diamond Head at Blewett Pass on Thursday reported many wind scoured areas with previous wind transport primarily to W slopes. The 12/17 PWL was found at 30 cm down, but was not reactive. Facets at the base of the snowpack were not giving test results.

Tom Curtis was out again on Friday on Mt Cashmere and on a W aspect near treeline and he found the 12/17 PWL at 55 cm giving a PST 37/100 End. He noted some previous wind transport and cross loading on N-W-S aspects. Tom also found great skiing conditions in the trees. 

An observation via the NWAC observation page from Saturday continued to identify weak persistent grains near the base of the relatively shallow snowpack in the Mission Ridge area. While these layers were reactive in column tests, no recent avalanche activity has been observed involving these layers. 

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.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.