Southeast Mountains

The final pulse of snow and wind today is stressing weak layers that have been producing large and dangerous avalanches in the past few days.  Wind-loaded slopes are likely to produce more destructive natural avalanches today.    You can easily trigger a large avalanche from on, near, or below steep terrain, and natural avalanches could run into flat terrain from above you.  Travel in avalanche terrain is not recommended, especially below leeward start zones. You can safely enjoy the new snow by staying on slope angles less than about 30 degrees without overhead hazards.

The mountains picked up 2" to 8" overnight with similar snow totals expected today.  This new snow is relatively low-density compared to what we saw over the weekend. Thus, new storm slab formation may be limited.  Our biggest concern today is that the new snow is easily transportable by the 20 to 30 mph winds at alpine locations.  Wind transport will continue to stress buried weak layers that reached their tipping point over the weekend.  We have had limited visibility of high-elevation terrain this week, so there's a fair amount of forecaster uncertainty with how much avalanche activity today's wind loading will produce.  Avoiding travel on or in the runouts of leeward start zones is prudent given that more natural activity is expected.  Leeward start zones could produce very destructive avalanches that run far into their runouts, like this recent avalanche on Whetstone.  The threat of natural avalanches is lower in wind-sheltered terrain, but you can easily trigger a dangerous avalanche at all elevations today.  Terrain closer to and east of town has proven to be especially reactive to human triggers (see video), where slabs are ideal depths for human triggering and buried weak layers are most fragile.  

We're just starting to gather data on the patterns and characteristics of the ongoing avalanche cycle brought about by significant loading in the past week (Over 5" SWE at Schofield Pass and 2.5" of SWE at Mt. Crested Butte). The most obvious pattern, unfortunately, is that we have documented large avalanches breaking on almost every aspect and elevation. That’s because our mid-December facets, faceted crusts, and surface hoar layers formed around the entire compass.  On low-elevation, south-facing slopes near town, the faceted crusts and slabs are embedded in sagebrush and other vegetation, making avalanches less likely on those types of slopes.  Otherwise, all terrain is capable of producing a persistent slab today.  Another variable at play is the wind effects from the arctic blast prior to the big storm.  In some terrain, those previous winds either completely removed the snowpack, or damaged the weak layers that were forming at the surface (recall this video).  Preliminary observations suggest that the most wind-damaged slopes were less active during the cycle.  The spotty surface hoar event that occurred after the artic blast threw some jokers in the deck.  This all means that there’s spatial variability out there, and you would need to very carefully assess the snowpack structure on a slope by slope basis if you are considering avalanche terrain.