Avalanche Forecast Olympics

Date Issued: Valid Until:

Kenny Kramer,

Avalanche Forecast

Sun Jan. 27th · 6:00PM

Alpine

Danger Ratings Below Threshold

Treeline

Danger Ratings Below Threshold

Below Treeline

Danger Ratings Below Threshold

Problems

Alpine

Danger Ratings Below Threshold

Treeline

Danger Ratings Below Threshold

Below Treeline

Danger Ratings Below Threshold
The Bottom Line: Although the weather is quiet, the warm temperatures are maintaining some uncertainty regarding how recent colder snow interfaces are adjusting to the warming. Watch for deeper melting surface snow on steep sun-facing slopes sheltered from the wind.

Snow and Avalanche Discussion

Temperatures have been above freezing at Hurricane Ridge for the past three days. If you see signs that the snow is not adjusting well to the warming, such as glide cracks, cornice failures, larger avalanches, or wet snow that your boot sinks easily into, seek safer terrain.

The January 22-23 storm ended warm and likely formed a rain crust to approximately 5500 ft. Melt-freeze crusts should exist on most aspects to ridgelines following the several days of very mild temperatures and sunshine.

While Loose Wet avalanches will be unlikely on Monday, you might encounter wet snow on steep, rocky, sunny slopes. If you start experiencing roller balls or wet snow deeper than your ankle, adjust your aspect to find firmer and safer conditions.

We received another recent observation from the Olympic mountains. Low snow coverage below 4000' and evidence of many strong crusts throughout the snowpack told the story of multiple rain events in this area, as well as recent avalanches on lee slopes at higher elevations.

Right now we are forecasting without specific snowpack and avalanche observations from the Hurricane Ridge area due to the government shutdown. If you travel to the Olympic Mountains, please help your local forecast by submitting an observation.

Weather Forecast

Mon 28th Jan 13:28 - Kenny Kramer

Weather Synopsis for Monday night through Wednesday

A ridge of high pressure will remain centered offshore on Monday night and weak gradually through Wednesday, maintaining fair and dry weather. Surface high pressure has strengthened east of the Cascades Monday causing increasing easterly winds across the Cascade crest and through Stevens, Snoqualmie and White pass.  Surface high pressure and cooling easterly winds have strengthened a temperature inversion with below-freezing temperatures returning to the passes and lower elevation areas, especially along the east slopes.

Some high clouds will continue to spill over the ridge at times through Wednesday, however, plenty of sunshine will persist both Tuesday and again Wednesday.

The current weather pattern typically causes extensive low clouds and fog along the east slopes and valleys, however, a lack of sufficient low-level moisture is limiting clouds and fog to just patchy areas.

The moderate easterly winds Monday should gradually subside Tuesday through Wednesday, allowing for warmer temperatures.

The next approaching weather system expected to undercut the offshore ridge has been consistently forecast to move southward well offshore Tuesday and head towards southern California Wednesday, missing the region entirely. 

Regional Synopsis

Sat 26th Jan 09:00

The late January pause...

Now that we’re well into winter and in the midst of a prolonged period of quieter weather, this is a good time to assess the current snowpack. Most areas are hovering around 75% of average snowpack depth for the season to date. Many of this season’s storms have brought at least some rain to mid elevations at the passes and west of the Cascade Crest. Multiple periods of cool, clear weather formed persistent weak layers.

Icicles hanging off of a snow feature are evidence of recent rain and daily temperatures swings. Stevens Pass. Photo: Josh Hirshberg


Recent conditions

 A prolonged period of warm quiet weather followed a storm on January 22-23rd that impacted most of the region. This weather system changed snow at the surface of the snowpack, drove an avalanche cycle, and tested or changed the latest persistent weak layers. The storm ramped up late on the 22nd in most areas. Intense precipitation (mostly snow) fell by dark with strong wind and warming temperatures. In the early morning hours of the 23rd snow switched to rain at the passes and western zones. Cold air to the east maintained low-density snowfall at most locations well east of the crest. In some areas, especially east of the crest, a new weak layer may have been buried at the January 22nd interface.

Wet loose avalanches on Mt Herman, near Mt Baker from 1/23. Photo: Lee Lazzara


January 23rd avalanche cycle

The bulk of recently reported avalanche activity occurred on January 23rd with high precipitation rates and wind loading in the early morning hours or with liquid water in the snow from rain or warming and sun during the day.

At the passes and in the western zones, reported avalanches were generally running either at the new/old snow interface or within the new snow. Observers reported a mix of soft slab, wet loose avalanches from near and below treeline with a few reports of shallow slabs above treeline. As of January 24th observations at upper elevations have been limited, due to lack of visibility and access.

In the eastern zones at areas like Washington Pass, Icicle Canyon, and the Wenatchee Mountains, some reported slab avalanches were confirmed or suspected to have involved persistent weak layers. Most notable is the January 17th surface hoar/near surface facets. There were a few reports of widely propagating avalanches, up to destructive size 3. Wind loading was a factor in many avalanches that released at upper elevations. Observers reported a widespread point releases on steep sunny slopes in the new snow where skies cleared on the 23rd.

A highlighted crown of a slab avalanche in Wenatchee Bowl, adjacent to numerous loose avalanches. Avalanches ran on January 23rd in recently fallen snow. Stevens Pass. Photo: Josh Hirshberg


Persistent Weak Layers (PWLs)

The latest round of snow, rain, and warming that tipped the balance of the snowpack was a good test of existing persistent weak layers. While the ever-changing snowpack keeps us busy tracking changes, some trends are apparent.

West Slopes and Passes: With a few exceptions, persistent weak layers have gained enough strength through rounding or melt-freeze to no longer be a concern for triggering avalanches. The main uncertainty lies with the January 17th surface hoar at upper elevations near Stevens Pass. This PWL is no longer a concern below treeline or in other zones. It appears that surface hoar generally wasn’t a player in avalanche activity near and west of the Cascade Crest. At low elevations, it has either been wetted by rain or is capped with crusts and moist snow. There’s reason to prioritize other issues, like challenging travel conditions, below treeline.

A slab avalanche on 1/23 (likely ran on the January 17th surface hoar) in Varden Creek drainage, near Washington Pass. The crown extends out of the photo, over 300ft wide.


Eastern Cascades: Triggering avalanches on persistent weak layers is possible east of the Cascade Crest. How much of a concern and exactly which PWL depends on where you are, north to south and east to west, in the range. The January 17th surface hoar/near surface facets is the main concern in the upper snowpack. Areas of shallower snowpack that lie further east of the Cascade Crest will have weaker snow and more pronounced weak layers in the mid to lower snowpack. In the Wenatchee Mounains you may find another layer of surface hoar (January 3rd) in the middle of the snowpack as well as weak facets near the ground. In places, like Washington Pass, the January 22nd surface hoar may become an issue with future storms.

Problems