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Avalanche Forecast

Archived

Mar 12th, 2016–Mar 13th, 2016

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Mt Hood.

Rapidly changing weather and snow conditions are expected on Sunday at Mt Hood. Back country travel is not recommended in avalanche terrain near and above treeline.

Detailed Forecast

The timing and track of the incoming low pressure system remains pretty consistent among the numerical weather models.

The deep low pressure system should move across the northwest tip of the Olympic Peninsula and across south Vancouver Island Sunday afternoon and evening. This should bring stormy weather and heavy snow to the Mt Hood starting Sunday morning. A vigorous, strong front should rapidly cross the Mt Hood area and cause rapidly shifting winds Sunday afternoon.

The main avalanche problem Sunday should be increasing strong winds and increasing moderate to heavy snow rapidly building new wind slab on lee slopes. This is very likely to be northwest to southeast slopes. New storm slab should also be likely where there is rapidly accumulating new snowfall.

Dangerous avalanche conditions are expected Sunday and back country travel there is not recommended in avalanche terrain near and above treeline.

Snowpack Discussion

Weather and Snowpack

The nonstop active weather pattern continues to push a storm system through the PNW almost every day or two resulting in fluctuating snow levels and periods of very strong winds (100+ mph gusts have been seen at the Mt Hood Meadows Cascade Express station over the last 2 weeks).

A last storm arrived Wednesday bringing heavy snowfall/rain at rising temperatures and very strong S-SW ridge top winds. About 2 inches of water and 8 inches of snow was seen the the NWAC stations at Mt Hood Meadows and Timberline for the 2 days ending Thursday morning with much of the water in liquid form. 

A front on Saturday is causing west-southwest winds and there should be up to a few inches of new snow at Mt Hood by Sunday morning.  

The mid and lower snow pack at Mt Hood should be a stable mix of crusts and layers of moist and rounded snow crystals.

Recent Observations

On Wednesday morning, new extensive wind slabs were forming on lee slopes near and above treeline. Explosive control performed by Mt. Hood Meadows pro-patrol Wednesday produced widespread slab releases on wind loaded N-NE facing terrain with crown depths of 2 feet common. Storm slabs Wednesday morning changed to loose-wet avalanches by midday as temperatures rose and snow changed to rain below treeline. 

On Thursday, NWAC pro-observer Laura Green toured in the Mitchell and Heather drainages and found evidence of rain up to at least 6600 feet. Thin wind pockets were observed on lee slopes above treeline. A supportable rain crust did not make for good skiing, but on the plus side no avalanche problems were noted. Runnels were observed below 6000'. 

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.