On Tuesday February 7 at the Sandy REI is the next presentation of Know Before You Go - a free avalanche awareness program. Not much science, no warnings to stay out of the mountains, no formulas to memorize. In 1 hour, you will see the destructive power of avalanches, understand when and why they happen, and how you can have fun in the mountains and avoid avalanches.
Also - for those that enjoy podcasts - Doug Krause has an excellent new avalanche-related podcast appropriately named Slide. It is a nice combination of practical advice, snow science, as well as human factor issues.
As of 5 am, temperatures are in the low twenties in the central Wasatch. Winds are out of the west and south west, gusting in the teens and twenties at the mid and upper elevations. 2-4” of fresh snowfall was reported from Big and Little Cottonwood Canyons, as well as the Park City mountains, on Thursday. This small refresher improved skiing and riding conditions. This was the first snowfall since Thursday January 26; it has felt like an eternity.
Week in Review
Friday January 27 was a stunning bright and bluebird day, with several feet of fresh snow that had fallen the prior eight days. However, six human triggered avalanches were reported that day, primarily in the Park City mountains as well as Lambs Canyon and Summit Park in Parleys Canyon. These occurred in elevations ranging from 7600’ - 9400’ and on northwest through southeast aspects. The weak layers were either preserved surface hoar or near surface facets, buried down 2-3’ in the snowpack.
Trent produced an excellent video recap of the avalanche that occurred on Sound of Music in the Park City mountains on the 27th. This video describes the persistent weak layer, as well as efficacy of avalanche safety equipment.
On Sunday Jan 29 and well as Tuesday Jan 31, two additional human-triggered slides were reported, one on Murdock Peak on a northeast aspect at 7600, the other in Summit Park on a north aspect at 8200’. Both failed on a layer of preserved surface hoar buried down about 2'.
Otherwise, while the Salt Lake valley was mired in an atmospheric inversion, the mountains were warm and mostly sunny. This extended period of clear weather weakened the snow surface, leaving behind a layer of surface hoar and near surface facets on most sun-sheltered aspects, and a breakable sun and temperature crust on other aspects. Fortunately, moderate to occasionally strong winds early this week, as well as warm temperatures, have seemingly destroyed these weaknesses at the old snow surface. With a few inches of snow from Thursday, and more snow on the horizon, it will be important to evaluate the old snow surface for any preserved weak layers underneath any new snow.
January Alta Guard Summary 8700' (Thanks to Mark Sauer) You didn't just imagine it, January was a snowy month with 154" of snow with 13.3" of water. This is the 6th highest January snow/water on record. (Average is 91.5" with 8.6" of water.)
On Thursday observers were finding pockets of sensitive wind drifts and small cornices along upper elevation ridge lines from southwest winds. These were mostly shallow - up to 6”. Little wind affect was noted down off of the ridges. Others were finding sluffing in the new snow, but it required steeper angles (> 35 degrees). Otherwise no avalanche activity to report.