Current Conditions:
Blizzard conditions rage in the central Wasatch high country this morning with heavy snowfall and blustery winds. Overnight, the mountains from Ogden to Salt Lake picked up another 8-12” in the past 24 hours, pushing storm totals to 2-3’ over the two days. Densities are in the 6-8% range despite periodic graupling. The west to northwest winds along the ridgelines intensified this morning to 35-45mpg with gusts to the 60’s but this should ease off late morning as the disturbance moves through. Temperatures plummeted to the single digits and below zero above 11,000’.
Avalanche Conditions:
Avalanche workers this morning reported heavy drifting at most elevations and aspects with the gusty and swirly winds. For backcountry travelers that make it into the high country, human triggered slides in the new snow will be likely on all steep drifted slopes, with a very distinct possibility of some stepping down into the older, weaker snow layers. Mostly confined to mid and upper elevation northwest through north through east facing slopes, these larger slides may be greater than 3-6’ deep and more than a few hundred feet wide. Furthermore, these larger slides may be even more pronounced in the outlying areas, such as the Park City ridgeline, Mill Creek, and the Provo area mountains. Cornice dropping, test slopes, and conservative slope cuts should reveal some good information, but today’s not the day to hang it out.
Headlining the avalanche news from yesterday is a skier released slide in No-Name bowl off the Park City ridgeline, a north to northeast facing slope at about 9800’. Details are still filtering in, but it appears that with eleven tracks already on the slope, a skier released the entire bowl 3-5’ deep and possibly 600’ wide. The slide not only engulfed the skier, but his three partners waiting for him below. All were partially buried, with one near-complete burial, but everyone came out miraculously unscathed. Avalanche control work in both Big Cottonwood canyon and the Park City areas continue to pull out slides to the ground and up to 7’ deep in uncompacted terrain.
Bottom Line:
The avalanche danger is CONSIDERABLE with human triggered avalanches likely on steep drifted slopes, with the real potential for them to step down into older faceted snow. Naturals may be possible in upper elevation areas that received the most snow and wind. Avalanches may be triggered at a distance, and as evidenced by yesterday’s close call, tracks are not necessarily a sign of stability with the current snowpack.
Mountain Weather:
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