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

Apr 4th, 2016–Apr 5th, 2016

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

.

Cool weather early Tuesday should give way to warming and sunshine in the afternoon, increasing loose-wet avalanche potential on steep solar slopes. Areas of shallow wind slab may linger on lee aspects at higher elevations, mainly easterly facing. ? The avalanche danger will quickly decrease further east from the Cascade crest due to minimal new snow accumulation. 

Detailed Forecast

Showers should end by early Tuesday with increasing sun breaks, especially by afternoon Tuesday. Temperatures should remain cool Tuesday, with modest warming due to solar input by afternoon.

The shallow recent snow received Monday, in combination with moderate westerly winds may have built areas of wind slab on lee slopes, mainly easterly facing near and above treeline where extra caution is warranted.  Firm wind transported snow and snowpack cracking can be good signs of wind slab layers. 

Small loose wet avalanches, mainly involving any recent new storm snow from Monday and Monday night will be possible on any steeper solar slopes, especially during prolonged sunbreaks Tuesday afternoon. 

The likelihood of cornice failure will lower Tuesday due to cooler weather. However, cornice releases can be unpredictable during the spring so continue to be aware of the overhead hazard and that cornices can break much further back than expected along ridges.

Although not listed as an avalanche problem, large, powerful glide avalanches can release unexpectedly so avoid areas below steep unsupported slopes or rock faces.

Snowpack Discussion

Weather and Snowpack

A large upper ridge dominated the weather last week through early Sunday, resulting in very warm and dry weather. A spring avalanche cycle occurred in most areas over this stretch, likely peaking Thursday or Friday during the warmest temperatures and lightest winds. After a stormy March, the snowpack has undergone significant settlement and multiple melt-freeze cycles over the last week.

A front moved across the Cascades early Monday morning, resulting in a period of mostly light precipitation, cooling and moderate westerly crest level winds.  Precipitation transitioned from rain to snow as cooling occurred, forming a generally good bond to the old melt freeze crust.

Frequent March storms have built unusually large cornices along many ridges.

No persistent weak layers formed earlier this winter are layers of concern as we transition to a spring snowpack along the east slopes. 

Recent Observations

NWAC professional observer Tom Curtis was out on the Wenatchee Ridge near Lake Wenatchee Wednesday, 3/30 in the 2-4000 foot range and found many slopes melted out. On slopes still holding snow he found natural and easily triggered, loose wet avalanches on all solar slopes in the top 15-20 cm of snow.

Tom was out yet again on Mt Lichtenberg near Stevens Pass on Thursday and found widespread large natural loose wet avalanches on nearly all solar aspects with easy to trigger loose wet avalanches on non-solar slopes.

A report on Turns All Year for the Chiwaukums described big rollerballs and big resulting debris piles on Thursday.

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.