Expect to find wind slabs of varying thickness and hardness on east, north, northeast, northwest and cross loaded west aspects. You are most likely to find these slabs at or near the ridge tops or in exposed terrain above 7,000 feet. They are still relatively widespread in the upper elevations and range in sensitivity from touchy to unreactive. These slabs range in density between soft to hard, which means they may let you get well out onto them before they fail. Also, keep in mind that some of these wind slabs may be resting on a newer layer of buried surface hoar that was formed early last week, or even worse could step down to the buried surface hoar layer that formed in early January. As temperatures increase today and over the next few days some of these windslabs may become unstable as the snowpack warms. Overhanging cornices may also begin to fail with the heat. if you are on a slope and notice the snow changing, you will want to find cooler slopes or call it a day.
We currently have 2 different persistent layers that we are tracking: one is relatively shallow and the other relatively deep. Both layers are made up of either buried surface hoar or near surface facets and represent old surface snow that was subjected to the faceting process during periods of high pressure in between snow cycles. The deeper layer is the one that resulted in the large and fatal slide near Twin Lakes on Sunday and the substantial natural avalanche cycle that we saw following MLK day. It is becoming a deep instability problem that is increasingly hard to trigger and not very widespread but is probably unsurvivable if triggered. In hazard evaluation terms it is a LOW probability/HIGH consequence problem. Its current depth is between 2.5 and 3.5 feet down in the snowpack depending on the windloading on individual slopes. Unfortunately, this layer is likely to stay where it is for quite some time and Snowmobiles are more likely to trigger it than a skier. It is also very hard to predict where you will trigger it because of its non-uniform distribution across the larger area and even across individual slopes and small micro features. Shallow wind protected areas well below the ridge tops, areas around rocks or on slopes with rocks sticking out or barely covered that were mostly protected from the winds are our best description for where you might trigger it right now. If you avoid areas with complex or convoluted terrain with lots of varying snow thickness across a slope, you will eliminate a large portion of the risk of triggering this layer, better yet spend your time boondocking through more moderate terrain and leave the steeps alone right now.
The upper layer is also made up of faceted snow or preserved surface hoar that was the snow surface last week before our last round of snowfall. In addition, we are finding areas with substantial grauple layers that were deposited a week ago as the last significant storm entered our area. This upper layer is becoming more stable with time but is more likely to be triggered by skiers or snowmobilers with equal chance due to its proximity to the surface right now. It is also variable where you will find it and what it is comprised of based on the winds, and the type of precipitation that fell on top of it. Both of these layers are easily identifiable as a gray line or layer in the snow when you dig through them.
A warming trend will add a significant stress to the snowpack as layers begin to melt and add weight and water to the upper snowpack. Be aware that rapid warming is one of the main red flags and that these will be the warmest temperatures of the winter so far. Persistent weak layers have a tendency to reactivate when the snowpack initially begins to warm up. The possibility of natural and human triggered avalanches will increase with the temperatures over the next few days.
Watch for a warm up of the snow surface today. Wet/Loose activity and roller ball activity have been on the increase over the last 3 days and temperatures in the mountains are going to continue to climb. Be wary of sunny aspects as they warm today and over the next few days. Remember rapid warming is a red flag avalanche warning, pay attention to changing snow conditions as the Death Star turns up the heat.
That's right folks, it's almost time for our annual fundraiser...next Saturday at the Little Ski Hill from 6-9 ish. Spoiler alert: Beer from McCall's own SRB, Waverunner rental from Cheap Thrills and skis from Dynafit! Practice up with those beacons and get ready for some timed beacon races with great prizes. Family Friendly with night skiing and plenty of parking available on both sides of the highway. Thanks to all the donors that have supported us in the past and again this year!
The entire advisory area is seeing warming of the snow surface due to the warms temps and sunny skies. Roller balls, point releases, and tree bombs (all signs of warming snow) were witnessed in the afternoons on both Saturday and Sunday and will continue through this week. Be on the look out for these Red Flag indications of the snow surface warming as you are out traveling today. Objectives are best accomplished early in the day to avoid travailing in terrain where wet snow avalanches will be a concern.
Break out your sunblock. Sunny skies today with temps in the 40's at 7,000 feet. An inversion will persist keeping the valley slightly cooler than the mountains through the week. Next chance of precipitation is Saturday, but the large ridge currently over us could push any available moisture to the north of us.
This avalanche advisory is provided through a partnership between the Payette National Forest and the Payette Avalanche Center. This advisory covers the West Central Mountains between Hard Butte on the north and Council Mountain on the south. This advisory applies only to backcountry areas outside established ski area boundaries. This advisory describes general avalanche conditions and local variations always occur. This advisory expires at midnight on the posted day unless otherwise noted. The information in this advisory is provided by the USDA Forest Service who is solely responsible for its content.