Stevens Pass

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Update 07:00 April 11: Dangerous conditions have developed. The snowfall is beginning to stack up, and with it comes increased avalanche danger. Wind slabs may be reactive and become large at upper elevations. Wet loose avalanches may run far, and pack a punch. Stay tuned to the quickly changing conditions that you are likely to experience. Plan to step back, and travel with caution near steep slopes on Thursday. 

A solid spring storm is moving through that is already accumulating quite quickly. The avalanche danger is on the rise once again, and be prepared to evaluate quickly changing conditions on the fly. Strong April sun and daily warming will likely create large wet loose avalanches. If you venture above treeline, you may find colder, winter-like avalanche conditions from snow that fell since Friday. The April 5th interface is likely to be found 14" to 20" below the surface, and may still harbor cold winter-like layers. At mid and lower elevations most of the snow from the past week has been wetted and frozen at least once. Observers near Grace Lakes reported breakable, frozen surfaces and challenging travel on Monday. On Sunday, observers reported a widespread cycle of natural and triggered loose wet avalanches in the recent snow on steep slopes above 4,000ft and on all aspects. One slab avalanche occurred on an east aspect, 5,000ft near the ridge at Gemini Pass. The recent snow is sitting on crusts with underlying weak, wet snow.

Other considerations are 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, and rockfall may occur sporadically. 

Debris from a natural loose wet avalanche (D2), Lichtenberg Mtn, SW, 5,000ft. 4/7/2019. Photo: Josh Hirshberg

April 9th, 2019

Spring Conditions

The snowpack and weather have shifted solidly to spring-like conditions. A major warm-up started in mid-March with a prolonged period of strong sun and warm temperatures. This created a major difference between the snowpack on sunny slopes and that on shaded aspects. More recently, warm, wet, and sometimes weak spring storms have brought more rain than snow. The bulk of the precipitation with these storms focused on the southern forecast zones. Even so, mid-elevation rain established a dramatic snow line (about 4-4,500ft) below which the snowpack is minimal to non-existent in most zones. Going into the second week in April, intense snow and wind drove a prolonged period of High danger at Mt Hood.

A crown of a very large avalanche (D3+) above Mt. Hood Meadows resort. 04/08/2019. Photo Credit: Peter Moore.

Challenging Weather Forecasts

The Cascades have been experiencing unsettled spring weather with rain to many low and mid-elevation slopes and snow at upper elevations. Spring weather forecasts in the Cascades are notoriously challenging. With these storms, the weather models have been inconsistent and the accuracy has been limited to 12-24 hours, at best. A trend has been significant precipitation amounts for the Mount Hood area and other south-central Cascade volcanoes. 

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

Shrinking Snowpack

From the peak height of snow in mid to late February through early April, mountain weather stations in the 4,000-5,000ft range showed an average of 27% decrease in height of snow. The percentage decrease ranged from 22-29%. This year's spring snowmelt is much earlier than normal. If you’re 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. On upper elevation shaded slopes there’s still potential for large wet slab avalanches with prolonged warm temperatures or high elevation rain events.

A natural loose wet avalanche (D1), Lichtenberg Mtn, N, 4,850ft. 4/7/2019. Photo: Will Govus

Spring avalanche considerations

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

1. Can you trigger avalanches due to new snow?

   1. If so, would they be storm slabs or wind slabs? And where?

2. Can you trigger avalanches due to warming or rain?

   1. Will recent snow be warmed enough to result in loose wet avalanches?

   2. Will these avalanches be predictable point releases or more destructive wet slabs or gouging loose wet avalanches?

   3. What are the recent high and low temperatures and the forecasted temperatures during the time you’ll be in the mountains?

   4. 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?

Debris from a natural loose wet avalanche (D2), Lichtenberg Mtn, SW, 5,000ft. 4/7/2019. Photo: Josh Hirshberg

Other Considerations

In addition to daily avalanche hazard, the early snowmelt has created 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.

The last daily avalanche forecast for all zones will be issued for April 14th. Statewide mountain weather forecast and weekly avalanche condition advisories will continue through May. The weather station data is available year round. Keep checking the advisories and help us out by submitting observations when you are in the mountains.

Glide avalanches and holes opening up in rocky terrain on an east aspect of Mount Herman. 4/3/19 Photo: Andrew Kiefer