23-24

North side of Wolverine

Date
Activity
Skiing
Snowmobiling

Wind load on old crust, probably from Wednesday. 

Region
Cooke City
Location (from list)
Wolverine Peak

GNFAC Avalanche Forecast for Thu May 2, 2024

Snowpack and Avalanche Discussion

<p><span><span><span><span><span><span>NEW SNOW AND WIND LOADED SLOPES</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>Spring storms are notorious for depositing heavy amounts of snow in the mountains. Even with a generally stable snowpack throughout the advisory area, heavy and rapid loads of new snow will decrease stability. The main problems to look out for are avalanches breaking within the new snow, wind slabs, and loose snow avalanches. The likelihood of triggering an avalanche spikes during and immediately after snowstorms. New snow instabilities tend to stabilize quickly, but it’s a good idea to give fresh snow a day to adjust before traveling on steep slopes. New snow instabilities can be challenging to assess, and spring storms bond to old snow differently across aspects and elevations. Conservative terrain selection is essential during and immediately following storms. Avoid wind-loaded slopes and slopes steeper than 35 degrees for 24-48 hours after new snow and wind.</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>New snow can quickly change from dry to wet on a spring day, and stability can decrease rapidly with above freezing temperatures or brief sunshine. New snow may bond well early in the morning and then easily slide later. Wet loose slides are likely during the first above freezing temperatures or sunshine after a storm. Anticipate changes in snow stability as you change aspect or elevation and over the course of the day. An early start is always an advantage. Be ready to change plans or move to safer terrain at the first signs of decreasing stability.</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>WET SNOW AVALANCHES</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>Spring and wet snow avalanches go hand-in-hand. Above freezing temperatures, rain, and/or intense sunshine cause the snow to become wet and weak, and wet avalanches become easy to trigger or release naturally. Conditions tend to become most unstable when temperatures stay above freezing for multiple days and nights in a row. Avoid steep terrain, and be aware of the potential for natural wet avalanches in steep terrain above you, if you see:</span></span></span></span></span></span></p>

<ul>
<li><span><span><span><span><span><span>Heavy rain,</span></span></span></span></span></span></li>
<li><span><span><span><span><span><span>Above freezing temperatures for more than 24 hours,</span></span></span></span></span></span></li>
<li><span><span><span><span><span><span>Natural wet avalanches,</span></span></span></span></span></span></li>
<li><span><span><span><span><span><span>Rollerballs or pinwheels indicating a moist or wet snow surface,</span></span></span></span></span></span></li>
<li><span><span><span><span><span><span>Or if you sink to your boot top in wet snow.</span></span></span></span></span></span></li>
</ul>

<p><span><span><span><span><span><span>In general, if the snow surface freezes solid overnight, the snowpack will be stable in the morning and stability will decrease through the day as snow warms up. The snow surface hardness, rate of warming, duration of sunshine, aspect and elevation determine how fast stability will decrease through the day. Be aware that sunny aspects may have a wet snow avalanche danger while shadier slopes still have a dry snow avalanche danger. Getting off of steep slopes should be considered when, or before, the above signs of instability are present. Wet snow avalanches, whether loose snow or slabs, can be powerful, destructive and very dangerous. Conservative terrain choices, starting early in the day, and careful observations can keep you safe.</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>CORNICES</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>Cornices along ridgelines are massive and can break under the weight of a person. Prolonged above freezing temperatures and rain make them weaker and possibly break naturally. They can break off suddenly and farther back than one might expect. Cornice falls can also entrain large amounts of loose snow or trigger slab avalanches. Stay far back from the edge of ridgelines and minimize exposure to slopes directly below cornices. Regardless of whether a cornice triggers a slide or not, a falling cornice is dangerous to anyone in its path.</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>DISCLAIMER</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>It does not matter if new snow falls or not, avalanches will continue to occur until the existing snowpack is mostly gone. Always assess the slope you plan to ride with diligence and safety in mind. Do not let your guard down. Travel with a partner, carry rescue gear and only expose one person at a time in avalanche terrain.</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>Have a safe and enjoyable spring and summer!</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>Doug, Alex, Ian and Dave</span></span></span></span></span></span></p>

<p><span><span><span><span><span><span>For more spring travel advice see this&nbsp;</span></span></span></span></span></span><a href="https://www.mtavalanche.com/blog/transitions-spring-snow-avalanche-prob… our GNFAC forecaster blog.</span></span></span></span></span></span></p>

Upcoming Avalanche Education and Events

Hyalite Road Closure: Hyalite road is closed to ALL MOTORIZED VEHICLES until the morning of May 16. This is a regular annual road closure to reduce road damage during the spring thaw. Bicycle and foot traffic are allowed. Contact the Bozeman FS Ranger District for more info.

Rider/skier triggered avalanche

Sheep Mountain
Cooke City
Code
SS-ASu-R2-D1.5-I
Elevation
9500
Aspect
NE
Latitude
45.07220
Longitude
-109.92800
Notes

From email 5/1/24: "Hi crew. I triggered a soft slab avalanche on the North side of Sheep Mountain today. D1.5 200’ wide ran 200’.  Crown was 6-12’’ deep. I was able to ride out of it and anchor in a safe spot. 

It broke on our 7th lap and we had seen no signs of instability prior to the avalanche but wind loading was occurring and obvious. The avalanche broke and on a dirty crust that formed during a rain event last week."

Number of slides
1
Number caught
0
Number buried
0
Avalanche Type
Soft slab avalanche
Trigger
Skier
Trigger Modifier
u-An unintentional release
R size
2
D size
1.5
Bed Surface
I - Interface between new and old snow
Problem Type
Wind-Drifted Snow
Slab Thickness
10.0 inches
Slab Width
200.00ft
Snow Observation Source
Slab Thickness units
inches
Single / Multiple / Red Flag
Single Avalanche
Advisory Year

From email 5/1/24: "Hi crew. I triggered a soft slab avalanche on the North side of Sheep Mountain today. D1.5 200’ wide ran 200’.  Crown was 6-12’’ deep. I was able to ride out of it and anchor in a safe spot. 

It broke on our 7th lap and we had seen no signs of instability prior to the avalanche but wind loading was occurring and obvious. The avalanche broke and on a dirty crust that formed during a rain event last week."

Cooke City, 2024-05-01

Rider/skier triggered avalanche

Date

From email 5/1/24: "Hi crew. I triggered a soft slab avalanche on the North side of Sheep Mountain today. D1.5 200’ wide ran 200’.  Crown was 6-12’’ deep. I was able to ride out of it and anchor in a safe spot. 

It broke on our 7th lap and we had seen no signs of instability prior to the avalanche but wind loading was occurring and obvious. The avalanche broke and on a dirty crust that formed during a rain event last week."

Region
Cooke City
Location (from list)
Sheep Mountain

Signs of stability at BBowl

Date
Activity
Skiing

Toured up to Bradley's Meadow, and found about 6 inches of moderate density snow sitting on a thin M/F crust with wet snow underneath the pack. 

Snow seemed well bonded and did not see any natural slides up on ridge. Not much sun was out, and it was snowing until 12 p.m. 

Region
Bridger Range
Location (from list)
Bridger Bowl
Observer Name
M. Standal