18-19

Skier triggered loose new snow at Bridger

Bridger Bowl
Bridger Range
Code
L-AS-R2-D1.5-I
Elevation
8400
Aspect
E
Latitude
45.81580
Longitude
-110.92900
Notes

Skiers easily triggered loose snow avalanches of the 3-5” of new snow. This morning (4/27) on the Bridger Ridge. Photo: @smooneyski

Number of slides
1
Number caught
0
Number buried
0
Avalanche Type
Loose-snow avalanche
Trigger
Skier
R size
2
D size
1.5
Bed Surface
I - Interface between new and old snow
Problem Type
New Snow
Slab Thickness units
centimeters
Single / Multiple / Red Flag
Single Avalanche
Advisory Year

GNFAC Avalanche Forecast for Fri Apr 26, 2019

Snowpack and Avalanche Discussion

<p>This weekend avalanches will be mostly confined to new snow that falls. These could be wet or dry loose slides, or slabs of new and wind-drifted snow. The snowpack is mostly frozen and stable this morning due to a light freeze under clear skies last night. Today before new snow falls, shallow wet slides are possible if rain or warm temperatures melt the snow surface.</p>

<p>The safest travel is on slopes with a supportable, dry or frozen surface. Anticipate dry new snow stability to decrease with wind, sun or above freezing temperatures. Be cautious of steep slopes if new snow is cracking, blowing and drifting, becoming moist or wet, or avalanching naturally. Be aware of deeper wet slides if the snowpack doesn’t freeze overnight, or if there is heavy rain. If you sink to your boot top in wet snow this is a sign deeper wet slides are possible.</p>

<p>Spring weather can quickly change between rain, snow, sun and temperatures above and below freezing. Snow stability can change rapidly from day to day and hour to hour. Now is just as important as ever to be diligent with snowpack assessment and choose terrain carefully (<a href="https://www.youtube.com/watch?v=foYa455ltOg&amp;list=PLXu5151nmAvRNl9ku…;). See below&nbsp;for more spring snowpack and travel advice.</p>

<p>If you get out and have any avalanche or snowpack observations to share, contact us via our <a href="https://www.mtavalanche.com/node/add/snow_observation">website</a&gt;, email (<a href="mailto:mtavalanche@gmail.com">mtavalanche@gmail.com</a&gt;), phone (406-587-6984), or Instagram (#gnfacobs).</p>

<h3><strong>GENERAL SPRING SNOWPACK AND TRAVEL ADVICE</strong></h3>

<p>Spring weather can be highly variable and create a mix of avalanche problems to watch out for. Snow conditions and stability can change drastically from day to day or hour to hour. Anticipate rapid change and plan accordingly. Abundant snowfall over the winter with more spring snow to come makes avalanches possible into summer.</p>

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

<p>Spring storms are notorious for depositing heavy amounts of snow in the mountains. Even with a deep and 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 new snow a day to adjust before hitting big terrain. New snow instabilities can be difficult to assess, and spring storms bond to old snow differently across aspects and elevations. Conservative terrain selection is essential during and immediately following storms. Wind loaded slopes and slopes steeper than 35 degrees should be avoided for 24-48 hours after new snow and wind.</p>

<p>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 immediately 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.</p>

<p>WET SNOW AVALANCHES</p>

<p>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 make wet avalanches 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 potential for natural wet avalanches in steep terrain above you, if you see:</p>

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

<p>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. See Alex’s recent <a href="https://www.youtube.com/watch?v=foYa455ltOg&amp;list=PLXu5151nmAvRNl9ku…;, and this <a href="https://www.mtavalanche.com/blog/transitions-spring-snow-avalanche-prob… more spring travel advice.</p>

<p>CORNICES</p>

<p>Cornices along ridgelines are massive and can break under the weight of a person (<a href="https://www.mtavalanche.com/images/19/large-cornice-near-cooke-city"><s…;). Prolonged above freezing temperatures and rain make them weaker and possible to 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.</p>

<p>DISCLAIMER</p>

<p>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.</p>

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

<p>Doug, Eric, Alex, and Ian</p>

GIVE BIG GALLATIN VALLEY

May 2-3 from 6pm-6pm. Give Big Gallatin Valley is a 24-hour online and live celebration of giving created to connect generous community members with the causes they care about most. Here is the link for more info and to support the Friends of the Avalanche Center during this event. Presented by the Yellowstone Club Community Foundation, and powered by the Bozeman Area Community Foundation.

Wet slabs near Cooke City

Crown Butte
Cooke City
Code
WS-AM-R2-D2-O
Elevation
9500
Aspect
NE
Aspect Range
NE-E-SW
Latitude
45.05840
Longitude
-109.96300
Notes

Several similar slides WS-R2-D1.5/2 were observed on 4/20/19. Many probably triggered by snowmobilers. At lower elevations natural slides were breaking to the ground. Several larger crowns were observed near Goose Lake on 4/23/19.

Multiple Avalanches
Number caught
0
Number buried
0
Avalanche Type
Wet slab avalanche
Trigger
Snowmobile
R size
2
D size
2
Bed Surface
O - Old snow
Problem Type
Wet Snow
Vertical Fall
300ft
Slab Width
100.00ft
Slab Thickness units
centimeters
Single / Multiple / Red Flag
Multiple Avalanches
Advisory Year