Avalanche Forecast

Issued: Apr 5th, 2019 11:00AM

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

Snowfall and gusty winds will combine to create wind slab instabilities on Saturday. Expect quickly changing conditions, and increasing danger as the day progresses. A potentially very wet and strong storm may impact the area on Sunday, further increasing the danger. 

Summary

Discussion

Snow and Avalanche Discussion:

It is turning back to winter in the high country. A stormy weekend is on tap, with avalanche danger on the rise. For Saturday morning, you may find a good overnight refreeze at the lower elevations. Cooling temperatures and increasing winds with some more snow at higher elevations may create wind slabs to be careful of. Dangerous conditions look to develop by Saturday night/Sunday in the mountains with potentially very heavy snowfall and rain. There is some uncertainty with the weather forecast, but if it all pans out, another round of heavy precipitation with warming temperatures and very strong winds are headed our way on Sunday. Large avalanches may become very likely, and may run to lower elevations. 

Previously, our avalanche problems have been driven by warm temperatures and a melting snowpack. On April 1st, an observer in the Eightmile Lake area found a very large recent wet loose slide off the west face of Colchuck Peak that may have been initiated by rockfall. See photo below. This is an example of the weak nature of the melting snowpack. If something large does initiate a slide, lots of snow may entrain on the way down. Weak and unsupportable wet snow has been found in many areas, especially in shallow areas near rocks. Be sure to consider all the hazards that come with spring in the mountains. Factor in a good margin for error as hard to predict events like cornice fall, glide avalanches, icefall, rockfall, and a general “shed cycle” in the mountains have been ongoing. 

Very large loose wet slide that gouged down to the ground, and may have been initiated by rockfall. Beneath the west face of Colchuck Peak. Observed on April 1, 2019.

Snowpack Discussion

April 3rd, 2019

Spring snowmelt

The snowpack in much of the Cascades has changed dramatically in the past two weeks. The weather has shifted solidly to spring-like patterns. The spring warm-up started in mid-March with a prolonged period of relatively clear skies and warm temperatures. Moving into April, we’re seeing periods of unsettled spring weather bringing rain to many low and mid-elevation slopes and snow to upper elevations.

Very bare southeast aspects of Rock Mtn/Nason Ridge. April 2nd. Photo: Josh Hirshberg

Since the peak height of snow in mid to late February, mountain weather stations in the 4,000-5,000ft range show an average of 27% decrease in height of snow. Looking at weather stations in nearly every zone, the percentage decrease ranged from 22-29%. This year's spring snowmelt is much earlier than normal. Traveling in the mountains the loss of snow coverage is most noticeable on southerly, sun-exposed slopes and below 4,000ft. On northerly aspects and slopes above 5,500ft, the snowpack has seen less dramatic changes and has even maintained some dry layers.

NWAC climatological snow depth data from April 1st. You can view it on our website here.

Spring avalanche considerations

As you head into the mountains there are a few questions to ask yourself common to spring avalanche conditions:

  1. Is there any recent snow accumulation that could cause avalanches? If so, what kind of avalanches could you trigger? And where?

  2. What are the high and low temperatures of the past 24 hours as well as the forecasted temperatures during the time you’ll be in the mountains? Could these create weak, wet snow surfaces?

  3. How is the cloud cover contributing to the melting or freezing of surface snow? Did clear skies allow for a sufficient overnight freeze? Will the sun be strong enough to weaken surface layers?

Glide avalanches and holes opening up in rocky terrain near Mount Herman. Photo: Andrew Kiefer

Other considerations

In addition to daily avalanche hazard, the early snowmelt is creating some other travel considerations. Some roads and lower elevation slopes may not have enough continuous snow coverage for travel on snow machines. Holes melted around rocks, trees, and creeks could create a fall hazard. When nighttime temperatures and cloud cover allow for surface freezes, bring appropriate equipment to mitigate slip and fall hazard on steep slopes.

We are approaching the end of our daily avalanche forecasting season. The mountain weather forecast will continue into the spring, and the weather station data is available year round. Keep checking the forecast for conditions updates on the end of season information.

Problems

Wind Slabs

An icon showing Wind Slabs

A bout of heavier precipitation with snow levels at around 6,000ft on Friday night may have created small wind slabs in alpine terrain. Another round of snow may arrive early on Saturday, with snow levels dropping to around 4,000ft. Gusty winds from the southwest or west will quickly transport the new snow into thicker drifts on lee sides of ridges and gullies. Be on the lookout for these to form especially at higher elevations, where significantly more recent snow may accumulate. If you find recently formed drifts or instability such as long cracks from underfoot, avoid steep wind loaded features. 

If the sun is out in the morning, be careful of steep east and south facing slopes, as loose wet avalanches may run with warming of the new snow. 

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: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 1

Valid until: Apr 6th, 2019 11:00AM