Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 7th, 2015–Feb 8th, 2015

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

Regions

.

Expect a decreasing avalanche danger Sunday with a break between systems. Watch for areas where more significant new snow has accumulated, mainly above treeline where new storm and wind slab are more likely. 

Detailed Forecast

A break between systems is expected during the daylight hours Sunday. This should give time for any recent shallow storm slab or wet new snow to settle and possibly refreeze to form new surface crust layers. This should allow for a slightly decreasing danger at higher elevations where more recent snow may have accumulated. Watch for wind transported new snow on some higher elevation lee slopes, mainly NW-SE facing   

Remember, due to the unseasonably low snowpack especially at lower elevations, numerous terrain hazards such as open creeks, partially covered rocks and vegetation are widespread.  

Snowpack Discussion

Periods of light snowfall were this week east of the crest with more snowfall at higher elevations in the northeast and central east zones. Steady but generally light precipitation was seen during the day Thursday with a gradual warming trend that continued into Friday. The snow level hung around 5500 feet in the northeast Cascades for most of Thursday night with snowfall accumulation likely in the 6-10 inch range in the Washington Pass area before likely mixing with light rain Friday. Much less new snow was reported in the Stuart range and Mission Ridge area above 6500 feet Friday.  Slight cooling with a frontal system Saturday has deposited an additional about 2-4 inches of snow above about 4-5000 feet. 

Observer, Tom Curtis traveled to Dirty Face peak above Lake Wenatchee Saturday. Shallow wet snow was accumulating above about 4800 feet where some storm and wind slabs where developing through the day near and above treeline while wet snow avalanches were possible below treeline.  There were no natural avalanches or instabilities observed with minimal wind slab developing along ridges from 5400 feet and above. The mid January crust layer we have been tracking was now poorly defined with no results from several stability tests performed. The new storm snow was only a few inches an was limiting the avalanche potential. 

NWAC pro-obs and North Cascade Guides, report last week in the northeast and central east zones have the January 15th facet/crust layers at 40 cm-1 m below the surface with the facets starting to turn to rounded grains and not reactive or not releasing in pit tests. It thus appears the January 15th facet/crust layers are strengthening and stabilizing. This problem has been removed from the central east zone forecast, but retained in the northeast zone until more information becomes available following this storm cycle.

Other private groups in the Washington Pass area on February 2 and 3 report some upside down densities in the recent snow from earlier in the week and natural and ski cut loose dry avalanches. 

Jeff Ward was in the Stuart Range Friday and found small but sensitive, loose wet avalanches naturally and skier triggered above about 6500 ft. Below this elevation, there was not enough new snow for wet loose danger and the most recent crust had not significantly softened. In the area traveled, the rest of the pack was consolidated and the Jan 15th layer was non-reactive in snowpit tests.

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.