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Avalanche Forecast

Archived

Jan 7th, 2018–Jan 8th, 2018

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

Regions

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Wind slab may be found on lee slopes near and above treeline, potentially extending into the below treeline depending on the local rain/snow line Sunday night. Small loose wet avalanches will remain sensitive to human triggering on Monday and possible on any steep slope regardless of aspect near and below treeline. Even small avalanches may travel further than you expect due to the 1/5 crust providing a firm sliding surface, so avoid steep terrain exposed to terrain traps.

Detailed Forecast

There is more uncertainty in the Mt. Baker forecast regarding how much new snow and/or rain will occur Sunday night. A warming trend with light to occasionally moderate precipitation is forecast to occur through early Monday morning, followed by a drying and likely partial clearing trend late morning through the afternoon. Freezing levels will be on the mild side. 

Wind slab may be found on lee slopes near and above treeline, potentially extending into the below treeline depending on the local rain/snow line Sunday night. Approach lee slopes with caution on Monday, watching for signs of recent or active wind transport.  The Considerable rating has been added to the above treeline band due to the increased possibility of larger wind slabs recently formed at higher elevations. 

A natural loose wet avalanche cycle should have occurred Sunday night in many elevations and areas. Loose wet avalanches will remain sensitive to human triggering on Monday. Loose wet slides should be small in size, but possible on any steep slope regardless of aspect near and below treeline. 

Shallow storm slabs will be listed as an avalanche problem in the Mt. Baker zone but they should quickly become stubborn to triggering as the day progresses. 

Small avalanches may travel further than you expect due to the 1/5 crust providing a firm sliding surface, so avoid steep terrain exposed to terrain traps.

Early season hazards still exist. Many creek beds have still not filled in for the winter.

Snowpack Discussion

On Sunday, light precipitation that began as light snow during the morning had mixed with light rain or freezing rain at lower elevations of Snoqualmie Pass and at Paradise on Mt. Rainier by late morning or early afternoon. Light snowfall accumulated at Mt. Baker and Stevens Pass through the afternoon. Winds were transporting new snow and building fresh but thin wind slab in the Mt. Baker area, near tree-line at Paradise in some near treeline areas of Snoqualmie Pass. Any new or recent snow overlies the 1/5 rain or freezing rain crust. 

Below the 1/5 crust, reports indicate a strong upper snowpack with no notable layers of concern and a multitude of crusts formed over the last two weeks. 

Observations

North

NWAC pro-observer Lee Lazzara was out in the Bagley Lakes area on Sunday.  Lee found gusty winds transporting new and recent snow onto various aspects and forming thin but sensitive wind slab through the early afternoon well down into the below treeline band. The 1/5 rain crust was ski supportable. Visibility was poor but glide cracks had re-opened on some steep rock faces due to the heavy rain event that ended Friday.  No new avalanche activity was observed. 

Central

NWAC professionals traveled in both the Snow Lake and Kendall Peak areas of Snoqualmie Pass on Sunday. Thin wind slab, up to 8" (20 cm), was building on a north aspect above Snow Lake at 4600 ft and reactive in column tests, failing on the 1/5 crust as of mid-day.  In the Kendall area, 1-4" of snow was reported above the 1/5 crust. Little active snow transport was observed to ridgecrest.  A thin rain or freezing rain surface crust was forming later in the day.  No new avalanche activity was observed.   

NWAC pro-observer Jeremy Allyn was in the Smithbrook/Rainy Pass area east of Stevens Pass on Sunday. About 3-4" of recent and new snow was well bonded to the 1/5 crust which was semi-ski supportable. Travel conditions were difficult. No new avalanche activity was observed. 

South

A professional in the Paradise area Sunday reported a switch form snow to freezing rain/ice pellets by late morning. This trend likely continued into Sunday afternoon as light to moderate precipitation produced no new snow at the Paradise weather station. As of mid-day Sunday, 4-6 inches of recent and new snow was well bonded to the 1/5 crust with a thin freezing rain crust noted at the surface. Some wind transport was occurring near treeline above 6000 feet due to moderate west winds. No new avalanche activity was observed. 

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.

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.