17-18

GNFAC Avalanche Advisory for Thu Feb 8, 2018

Snowpack and Avalanche Discussion

<p>It has snowed eleven out of the past twelve days around Cooke City and winds have been moderate to strong out of the west&nbsp;(<a href="https://www.mtavalanche.com/weather/wx-avalanche-log">weather log</a>). The relentless combo of snow and wind has pushed many slopes past their breaking point. A large and destructive natural avalanche off Woody Ridge on Tuesday is a prime example of what’s possible (<a href="https://www.mtavalanche.com/images/18/east-woody-ridge-avalanche"><stro…;). A foot of snow overnight and more today will only make conditions more unstable. Until the snowpack gets a breather, the best option will be to avoid avalanche terrain including avalanche runout zones (<a href="https://www.mtavalanche.com/images/18/sheep-mountain-avalanche"><strong…;).</p>

<p>Today, natural and human triggered avalanches are likely and the avalanche danger is rated <strong>HIGH</strong> on all slopes.&nbsp;</p>

<p>Bracket Creek Snotel site in the northern Bridgers has picked up over 3” of <a href="https://www.nrcs.usda.gov/wps/portal/nrcs/detail/or/snow/?cid=nrcs142p2… water equivalent</a> over the past four days. What’s unusual is Bridge Bowl has picked up roughly half that amount. The bottom line is – the sheer volume and weight of the new snow is putting a tremendous amount of stress on the snowpack. Wind loaded slopes will be the most prone to avalanches, but non-wind slopes remain suspect. We know the Bridger Range has a generally strong snowpack (<a href="https://youtu.be/UeRbanc6b3c"><strong>video</strong></a&gt;), but 3” of SWE in four days is enough expose any weakness. I wouldn’t be surprised if large&nbsp;natural avalanches occur, mainly in the northern part of the range. With more snow and wind on the way, the snowpack will remain on edge.</p>

<p>For this reason, the avalanche danger is rated <strong>CONSIDERABLE</strong> on all slopes.</p>

<p>Hyalite and Big Sky have received enough snow and wind to keep the avalanche danger elevated, mainly on wind loaded slopes. Overnight, winds blew 20-40 mph out of the west-southwest, which likely formed dense slabs in leeward terrain. Warm temps will keep wind slabs stubborn today, but they still can’t be trusted. These conditions also facilitate rapid cornice growth. Watch out for and avoid slopes beneath large cornices and give them a wide distance along the ridgelines.</p>

<p>Today, dangerous avalanche conditions exist on wind loaded slopes which have a <strong>CONSIDERABLE</strong> avalanche danger. Non-wind loaded slopes have a <strong>MODERATE</strong> avalanche danger.</p>

<p>The southern mountains haven’t received as much snow as the northern ranges. <a href="https://www.mtavalanche.com/weather/stations/carrot-basin">Carrot Basin</a> Snotel site in the southern Madison Range is showing .4” of SWE over the past three days while <a href="https://www.mtavalanche.com/weather/stations/madison-plateau">Madison Plateau</a> near West Yellowstone is showing .1” of SWE. Although snow amounts are less, buried surface hoar two feet deep and moderate to strong winds out of the west will present a few different problems today.</p>

<p>Watch out for wind loaded slopes near the ridgelines and avoid areas around large cornices. Also keep an eye out for surface hoar buried two feet deep. Yesterday, my partner and I rode in the Taylor Fork and got this layer to propagate consistently in stability tests (<strong><a href="https://www.youtube.com/watch?v=CFzhlPk5DZw&amp;list=PLXu5151nmAvQSYtIf…;). Doug and Alex also got unstable results on this layer near Hebgen Lake earlier in the week (<a href="https://youtu.be/2mj4jkCkEpc"><strong>video</strong></a&gt;).</p>

<p>Wind loaded slopes and buried weak layers make human triggered avalanches possible and the avalanche danger is rate <strong>MODERATE</strong>.</p>

<p>If you get out and have any avalanche or snowpack observations to share, drop a line 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>

White Heat Tracks Project seeks your input

The aim of the White Heat Project is to generate new and usable knowledge on risk-taking behavior, and on factors behind decision errors in avalanche terrain in particular. The White Heat Tracks project is an extension to the previous "SkiTracks" project, and is a collaboration between a group of researchers at UiT The Arctic University of Norway, in Tromsø; Montana State University, in Bozeman, USA; and Umeå University, in Umeå, Sweden.

GNFAC Avalanche Forecast for Wed Feb 7, 2018

Snowpack and Avalanche Discussion

<p><u>Cooke City</u></p>

<p>Yesterday a large avalanche was triggered by a cornice on east Woody Ridge south of town. The wind-loaded slope broke up to 10’ deep at the ridgeline (<strong><a href="https://www.mtavalanche.com/images/18/east-woody-ridge-avalanche">photo…;). The mountains have gotten over 4’ of snow in the last 5 days with wind loading slopes even more (<strong><a href="https://www.mtavalanche.com/images/18/sheep-mountain-avalanche">photo</…;). The slide on Woody was large and destructive and it is still possible for similar avalanches to occur. Wind loads are found near ridges, and not just on east-facing slopes from west winds: they will be found on many aspects underneath cornices and along ridges where winds cross-loaded and drifted snow into gullies. On slopes without a wind load it’s possible to trigger a slide within the new snow or on a weak layer buried underneath it. For today, the avalanche danger is rated <strong>CONSIDERABLE</strong> on wind-loaded terrain and<strong> MODERATE</strong> elsewhere.</p>

<p><u>Bridger Range</u> <u>Northern Madison Range</u> <u>Northern Gallatin Range</u></p>

<p>In the Bridger Range about 2” of <a href="https://www.nrcs.usda.gov/wps/portal/nrcs/detail/or/snow/?cid=nrcs142p2… water equivalent</a> fell north of Bridger Bowl since Sunday night which has settled to 10” of snow depth. Yesterday, Eric and Gabrielle (our intern) rode and skied into the bowl below Naya Nuki and measured the water content and found relatively good stability which is outlined in their <strong><a href="https://youtu.be/UeRbanc6b3c">video</a></strong&gt;. West winds are gusting into the 50s and wind-loaded slopes are the main avalanche concern. There has been snowfall in the northern mountains every day for the last 8 days (<a href="https://www.mtavalanche.com/weather/wx-avalanche-log">weather log</a>) and today’s winds have drifted this snow and increased the avalanche danger. On non-wind-loaded slopes the stability is good, but with all the steady snowfall avalanches are still possible. For today, the avalanche danger is rated <strong>CONSIDERABLE </strong>on wind-loaded slopes and <strong>MODERATE</strong> on all others.</p>

<p><u>Southern Madison Range</u> <u>Southern Gallatin Range</u> <u>Lionhead area near West Yellowstone</u></p>

<p>The southern mountains, including the West Yellowstone area, have a couple weak layers that are problematic. The first is a layer of surface hoar buried 1-2’ deep. It is not easy to spot in a snowpit wall, nor is it widespread. The second is sugary facets near the ground that is getting more stubborn to trigger. Both of these layers broke in our stability tests on Sunday when Alex and I skied near Hebgen Lake (<a href="https://youtu.be/2mj4jkCkEpc"><strong>video</strong></a>,<strong&gt; </strong><a href="https://www.mtavalanche.com/images/18/hebgentrapper-profile-4-feb"><str…;), so we decided to adjust our intended descent to a more conservative line. For today, the avalanche danger is <strong>MODERATE</strong> since avalanches are still possible.</p>

<p>If you get out and have any avalanche or snowpack observations to share, drop a line 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>

White Heat Tracks Project seeks your input

The aim of the White Heat Project is to generate new and usable knowledge on risk-taking behavior, and on factors behind decision errors in avalanche terrain in particular. The White Heat Tracks project is an extension to the previous "SkiTracks" project, and is a collaboration between a group of researchers at UiT The Arctic University of Norway, in Tromsø; Montana State University, in Bozeman, USA; and Umeå University, in Umeå, Sweden.

This natural avalanche occurred late in the day on Feb 5 (Mon) at 9800' on the northeast face of Sheep Mountain outside Cooke City. This was the tail end of the storm and on the day we issued an Avalanche Warning. Photo: J. Schutz

Cooke City, 2018-02-07