UDOT PLANNED AVALANCHE CLOSURES!!

Observation: Broads Fork

Observation Date
2/25/2022
Observer Name
Hardesty, Wilson, Nalli
Region
Salt Lake » Big Cottonwood Canyon » Broads Fork
Location Name or Route
Broads Fork
Weather
Sky
Overcast
Precipitation
Light Snowfall
Wind Speed
Calm
Weather Comments
Overcast and cold. No wind to speak of. Very light accumulations during the day.
Snow Characteristics
New Snow Depth
2"
New Snow Density
Low
Snow Surface Conditions
Powder
Snow Characteristics Comments
Best skiing and riding in two months, and not by a little. 10-14" of settled snow sits above the Jan/Feb drought layer PWL. Best and safest skiing exists on low angle shady aspects with no overhead hazard.
Red Flags
Red Flags
Recent Avalanches
Cracking
Collapsing
Poor Snowpack Structure
Red Flags Comments
We experienced very localized cracking and collapsing from 8000' - 8400' and went looking for a more cohesive slab. More below -
Avalanche Problem #1
Problem
Persistent Weak Layer
Trend
Same
Problem #1 Comments

We remotely triggered a 10-16" deep and 60' wide soft slab avalanche on a NE facing slope at 8700' that failed on the PWL. The slope was less than 35 degrees and so the "avalanche" ran perhaps a foot downhill at most.
It's likely that there may be a "sweet spot" for instability on northwest to east facing slopes at the mid-elevations. (West may also be at play but there is some uncertainty here.)
  • At the low elevations, very weak faceted snow exists but there doesn't seem to be much of a snow/wind load above to create a cohesive slab except in isolated terrain (that perhaps has seen more wind).
  • At the high elevations, weak faceted snow exists, but there is a lot of uncertainty as it is capped by spatially variable wind crusts.
  • At the mid elevations, very weak faceted snow exists and there are increasingly more places where the overlying slab has consolidated due to wind and settlement.
As we know, you need a few ingredients for an avalanche: a slab, a weak layer, a slope steep enough to slide, and a trigger.
Extended Column Tests - ECTPV (full propagation on isolation) from 8200-8400'.
Now the set-up is that the weak layers are easy to find: Jan/Feb drought layer facets (PWL) are buried 6"-2' (wind drifted areas) down and are LOOSE, grey, angular - the photos below make them easy to spot. Sometimes they sit above a crust, sometimes they don't.
Looking for a slab, however, can be very tricky for many reasons.
  • It may appear that there is no slab because much of the top snow is "powder snow"; but in reality it may be the couple/few inches of snow directly above the facets may have consolidated enough to propagate a slab avalanche.
  • Wind loading and snowfall patterns have been erratic and it is not necessarily possible to extrapolate one northeast facing slope at a certain elevation with another....even in the same drainage.
  • In essence, the weak layer hunting is easy and obvious - it's now that the slab hunting is tricky...and potentially dangerous.
Again, it may be that the mid-elevation polar aspects may be the sweet spot for avalanche activity.
Last point: conditions are variable, tricky, and dangerous in some areas. Collapsing and cracking may not be evident until you trigger the avalanche. Low angle skiing/riding (with no overhead hazard) is excellent without all the uncertainty and avalanche danger.
Video
Today's Observed Danger Rating
None
Tomorrows Estimated Danger Rating
None