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Avalanche Forecast

Archived

Jan 30th, 2014–Jan 31st, 2014

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Olympics.

The Bottom Line: Dangerous snow conditions are expected in parts of the Washington Cascades on Friday.

Detailed Forecast

Light snow showers should end Friday morning. Partial clearing should be seen Friday afternoon and night with continued cool temperatures.

There should be little change in snow conditions on Friday.

The top concern at Stevens and Snoqualmie and east of the crest will remain the persistent buried hoar frost slab layer. This layer will be found anywhere from a couple inches to a couple feet under the recent storm snow. Shooting cracks and whoomping are the strongest red flag observations for this persistent layer. Remember that this is also expected on small open slopes below treeline in the Stevens and Snoqualmie areas and east of the crest.

New wind slab is likely to remain on lee slopes above tree line on Friday. Watch for signs of wind transported snow above treeline. Temporary storm slab may survive on Friday on sheltered slopes near and below tree line on Friday. These are the more likely concerns in the Olympics, west of the crest and on the volcanoes.

Snowpack Discussion

Heads up folks because the avalanche picture has greatly changed in the Washington Cascades from the past couple weeks.

Dangerous persistent large hoar frost that formed during the latter part of the recent 2 week fair weather period has been buried in the Washington Cascades mainly at Stevens and Snoqualmie and east of the crest. By the end of Thursday this persistent layer will be found in these areas under anywhere from a couple inches to a couple feet of the recent storm snow.

Surface hoar layer with thin rimed crust before it was buried near Rainy Pass, about 4600 feet, 28 January, Photo by NWAC Observers Jeff Ward and Dallas Glass.

NWAC observers at Stevens and Snoqualmie today report snowpack whoomping, easy sudden collapse pit tests and Extended Column tests indicating propagation due to the persistent buried hoar frost layer including on your favorite go to slopes for such conditions - open low angle slopes below treeline. Here is a link to a video made today near Stevens Pass of tests of the buried surface hoar layer.

https://www.youtube.com/watch?v=IsYF79R6Rio

However a buried hoar frost layer is considered unlikely in the Olympics, west of the crest and on the volcanoes due to rain in those areas at the start of the recent storm. But it will be listed in these areas as an unlikely concern until there is confirmation one way or the other.

The recent storm is also expected to have built new wind slab on lee slopes above tree line. NWAC observers today also report new temporary storm slab on sheltered slopes near and below tree line in the Stevens and Snoqualmie areas. These should be the most important concerns in the Olympics, west of the crest and on the volcanoes.

At least the mid and lower snowpack consists mainly of crusts and melt form crystal layers. The low snow amounts on many south slopes and at low elevations and ample terrain and vegetation anchors are limiting the avalanche danger in those areas.

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.