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Avalanche Forecast

Archived

Jan 22nd, 2016–Jan 23rd, 2016

Alpine
Natural avalanches unlikely, human triggered possible.
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

Olympics.

Watch for recent shallow wind slabs that may have formed on the lee, northerly aspects below ridges, mainly near and above treeline.

Detailed Forecast

Cooling overnight Friday and Saturday with a weak system, depositing shallow new snow in showers Saturday with light winds, should all lead to an overall stabilizing snowpack. Any previously wet or moist surface snow may begin to form a thin surface crust, locally decreasing danger. Further continued snowpack settlement should also allow for an improving trend.

Watch for recent shallow wind slabs that may have formed on lee, northerly aspects below ridges.

Snowpack Discussion

A few inches of moist to wet snow accumulated Monday through Wednesday, with the Waterhole NRCS snowdepth slowly rising to 76 inches through mid-week.  

A wet and warm frontal system drenched the Olympics Wednesday night and Thursday with snow levels rising well above Hurricane Ridge, before cooling and depositing about 4 inches of snow by Friday. This caused a loose wet avalanche cycle on steeper slopes in all elevation bands, reported by Matt Schonwald from observation gathering Friday, January 22. 

Matt reported generally stable surface snow conditions with no layers of concern in the BTL and NTL elevation zones. Overall the snowpack consists of a few inches of saturated snow, well bonded to supportive dryer old snow. Stability tests were all negative. Some transport of loose surface snow was seen being deposited on the northerly facing terrain below ridges, but no distinctive wind slab had formed as of Friday afternoon. 

Hurricane Ridge weather station update: NWAC forecaster Garth Ferber was at Hurricane Ridge Thursday and with the help of NPS IT staff, our weather station is back online!  We appreciate everyone's patience and believe that our new internet connection to the weather station will prove to be far more reliable than the aging microwave it replaced last spring. 

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.