Register for an account and never miss a forecast again!
RegisterRegister for an account and never miss a forecast again!
RegisterMar 25th, 2016–Mar 26th, 2016
Stevens Pass.
While recent storm related avalanche problems will have greatly diminished by Saturday, isolated areas of wind slab may remain on lee N through SE slopes near and above treeline. Also, loose wet avalanches will be likely on steeper solar slopes, especially during prolonged periods of sunshine.
Variable cloud cover on Saturday will be accompanied by generally light winds and rising freezing levels. An incoming frontal system arriving Saturday night should spread high clouds over the area in the afternoon.
Recent storm related avalanche problems will have greatly diminished by Saturday. Isolated areas of wind slab may remain on lee N through SE slopes near and above treeline, but should generally be stubborn to human triggering. Firm wind transported snow and snowpack cracking can be good signs of wind slab layers.
Loose wet avalanches will be likely on steeper solar slopes, especially during prolonged periods of sunshine. Be aware of terrain traps where even a small loose avalanche could have unintended consequences in the wrong terrain.
Recently formed cornices have grown large. If traveling along ridgelines, be aware that cornices break much further back than expected and you don't want to go for a ride with a chunk of cornice. Despite the recent cool weather, cornice releases can be unpredictable during the spring.
Although not listed as an avalanche problem, glide avalanches can release unexpectedly so avoid areas below steep unsupported slopes or rock faces.
Weather and Snowpack
A low pressure system crossed the Northwest on Monday and Tuesday. NWAC stations along the west slopes accumulated a few inches above 4000 feet during this time. Light rain was seen on Wednesday in the below treeline band before a cold front swept through Wednesday night with moderate westerly transport winds continuing through Thursday afternoon for the south and central Washington Cascades. Orographic snow showers continued through Thursday night before tapering off Friday morning.
Post-frontal snow accumulations Wednesday night through Friday morning varied based on elevation, with only a few inches below 4000 feet and 6-21 inches above. The most snow was received at Paradise and Mt. Baker NWAC stations through Friday morning. New snow since Monday is generally well-bonded to a moist crust buried March 22nd.
Frequent March storms have built large cornices along ridges in many areas.
The mid and lower snowpack along the west slopes should generally be a stable mix of crusts and layers of moist and rounded snow crystals.
Recent Observations
Snoqualmie Pass avalanche professionals reported loose wet avalanches triggered by light rain running far on Wednesday in paths below treeline. Glide avalanches releasing to the ground off of rock surfaces were also reported near the same Snoqualmie Pass paths Thursday morning. NWAC professional observer Dallas Glass was in Kendall Peak area of Snoqualmie Pass Thursday and found small but sensitive wind slabs near treeline. Dallas also found loose snow concerns transitioning to shallow storm slab problem by mid-day with settlement and daytime warming.
The Mt. Baker pro-patrol reported only scattered and small soft storm slabs in area Thursday morning. Stevens Pass pro-patrol reported strong west winds had redistributed the new snow, but that the new wind slab was stubborn and generally nonreactive to ski cuts.
On Friday, Baker pro-patrol reported natural slab activity above treeline on Mt. Shuskan but only small loose wet releases in area and a generally right side up upper snowpack. A professional guide observation from the Snoqualmie Pass area Friday morning indicated generally well layered and bonded storm snow with increasing potential for loose wet avalanches by late morning.
Powerful glide avalanches remain possible in isolated terrain features such as on steep slopes with smooth bed surfaces and especially where the slabs are unsupported from below. These avalanches are not predictable in the sense that they are not tied to short term warming or rain events. We want to highlight the low likelihood-high consequence of this sporadic but ongoing avalanche hazard during this wet winter.