Date of Observation: 04/02/2021
Name: Zach Guy and Zach Kinler

Zone: Northwest/Southeast boundary
Location: Mt. Emmons
Aspect: North East, East, South East, West, North West
Elevation: 9500-12000′

Avalanches: A handful of small wet loose avalanches ran today, generally on northeast and some east aspects at all elevations. Skier triggered a couple of wet loose avalanches this afternoon below treeline on a northeast aspect. The slides gouged through most of the snowpack, large enough bury someone in a gulley (~D1.5). These were in steep, rocky terrain holding a shallow and weak snowpack that is just now becoming saturated.
Weather: Unseasonably warm: Highs reached mid 50’s at 10,000′ and 40 at 12,000′. Partly cloudy skies. Light ridgetop winds.
Snowpack: Several pits on E, SE, and W aspects N/BTL targeting wet slab concerns. Generally, slopes that are getting the most water right now have already seen a fair amount of water already and have moist or wet grains throughout the entire snowpack. Slopes where the snowpack has remained dry until the last few days have water in the upper few inches today. Water was pooling about 40 cm deep on a SE aspect NTL (the rest of the snowpack was moist), and pooling about 5 cm deep on a West aspect NTL (the rest of the pack was dry). At low elevations, the saturated snowpack became unsupportive (bottomless boot pen) by the afternoon on flat terrain. All but high northerly aspects or steep due north aspects at low elevations got wet today. Good, stable corn skiing this morning on southerly aspects until about noon, at which point the snow surface became increasingly mushy and we were able to trigger pinwheels and micro-sluffs. Northeast and northwesterly aspects were most active today for wet loose activity because the snow surface is just now transitioning from dry to moist or wet.

Date of Observation: 04/01/2021
Name: Zach Kinler Evan Ross
Zone: Northwest Mountains
Location: Southern Ruby Range
Aspect: East, South East, South
Elevation: 9,000′-12,600′

Avalanches: Observed several Wet Loose avalanches, both natural and human triggered. Size ranged from D1-D1.5 with activity primarily on steep East, South and Southwest slopes near and above tree line. While traversing the Ruby spine we encountered several large overhanging Cornices which had begun to pull back from the ridge. Two of these were triggered from dry ground on the ridge by simply “pole whacking” the gap.

We got a close look at the previously reported Cornice Avalanche on the SE flanks of Mt Owen. This was a big section of cornice that fell down and resulted in a large D2.5 avalanche. The cornice initially gouged close to the ground in steep rocky terrain, then appeared to run on March interfaces as dust layers can be seen on the bed surface.

Weather: It’s heating up! We skinned in t-shirts most of the day. Temps soared above freezing at all elevations today under abundant sunshine. Westerly winds were light at rideline.

Snowpack: We travelled primarily on sunny aspects from E-S near and above treeline. By 12:00, we observed several small natural Wet Loose avalanches on steep East aspects near tree line. As the day progressed, action moved to South aspects and eventually Southwest slope near and above treeline. While these avalanches were only entraining the upper few inches of wet snow, they were gaining momentum on larger slopes. Skiing off the ridge in the late afternoon, we choose to avoid our intended ski objectives that was south east facing above 12,oooft to due to the fact that we would be triggering loose wet avalanches and didn’t feel we could safely manage the problem on that terrain feature. While briefly hanging out on the bed surface of an old cornice avalanche you could actually hear water cascading somewhere. Sounded like you were standing next to a running water fountain.

Cornices, which have grown large throughout this season on certain leeward aspects, proved to be sensitive where large portions are overhanging ridges and are beginning to pull back from ridgeline. These babies are very unpredictable with some being resistent to cutting while others may be triggered by simply hitting the right spot or right time of day. These beasts were best managed by avoiding traveling on or below slopes where present.

Date of Observation: 04/01/2021
Name: Sam L

Zone: Northwest Mountains
Location: East face of mineral
Aspect: East

Avalanches: Skier triggered small wet loose. Slow and shallow, could have been worse with more exposure. Sorry no pic.

Weather: Clear and strong sun. Snow surface wet at 1030.

Date of Observation: 03/31/2021
Name: ben Pritchett

Zone: Northwest Mountains
Location: Carbon Peak
Aspect: North, North East, East, South East, South
Elevation: 9-11,000′

Avalanches: The slow trickle of large avalanches continues. In Whetstone Mountain’s Hidden Lake bowl, a broad (~250′ wide) section of very large cornice released around 12,200′ and triggered a Persistent Slab avalanche that broke at the ground on a northeast-facing slope. The avalanche looked fresh.

Weather: Chilly start following a strong freeze, warmed to just above freezing. Calm, and clear.

Snowpack: Near and below treeline south and southwest facing slopes have previously drained water to the ground. Little concern for future Wet Slabs. East to southeast-facing slopes near treeline could still pose a near-term Wet Slab concern. Thin slabs (30-70cm deep) rest on presently moist facets. Recently the meltwater has stopped within the slab, but if the melt rate picks up quickly these aspects would be most concerning first. North of east both near and above treeline I found a dry snowpack. Where the snowpack was deeper, the slab was fairly supportive and strong. Triggering a Persistent Slab avalanche remains unlikely, but consequences remain ugly. On these slopes with a dry snowpack, shallow areas remained spooky. In areas with less than around 3 feet of snow, boot penetration would go to the ground. I didn’t experience any collapsing, but I did two ECT’s and both produced hard propagating results on faceted weak layers, one at the ground, one in a very weak layer of large facets below the March storm snow.

Photos:

Date of Observation: 03/31/2021
Name: Evan Ross, Zach Kinler

Zone: Northwest Mountains
Location: Treasury
Aspect: North, North East, East, South
Elevation: 9,000-13,300

Avalanches: A few small wind slabs that had run over the last couple days. 1 one NE and a few on E to SE. All above treeline.

Weather: Cool northerly winds helped keep the heating in check. Clear Sky.

Snowpack: Normal caution on steep slopes or for small isolated avalanche problems. We considered trying to avoid a few trigger points when we were exposed to high consequence terrain. Thin surface slabs from the previous winds were stubborn, but still something we ended up managing a little in extreme terrain. Plenty of dry snow out there that is waiting to transition during the upcoming heatwave. On the way home there were lots of glossy-looking snow surfaces down at lower elevations.

Date of Observation: 03/30/2021
Name: Jack Caprio, Eric Murrow

Zone: Northwest Mountains
Location: Kebler Corridor
Aspect: North, North East, East, South East, South
Elevation: 9,500′-12,000′

Avalanches: No new avalanches observed

Weather:  Sky cover became partly cloudy in the morning with lots of sunshine by noon. Light northerly winds with moderate gusts. Warm temperatures near and below treeline out of the wind.

Snowpack:

We targeted wind-loaded slopes up to 12k in search of wind slab and persistent slab problems.  Recent wind-drifting in this area did not create much Wind Slab formation. We did step into steep N-facing, slightly wind-loaded alpine terrain. Near ridgeline, N/ NW wind events throughout the season had made the snowpack very shallow. The first 50 vertical feet down consisted of a very shallow mix of facets and thin windboard layers. After about 50 vertical feet the snowpack became deep and uniform again and we saw no signs of instability.

We briefly ascended a southeast-facing slope near treeline without much previous drifting and found HS between 70 and 100cm with a moist surface crust just supportive enough to carry skis, but not boots.  The snowpack below was weak isothermal snow to the ground without any slab.