UDOT PLANNED AVALANCHE CLOSURES!!

Forecast for the Provo Area Mountains

Drew Hardesty
Issued by Drew Hardesty on
Tuesday morning, December 18, 2018
While most terrain has an overall LOW avalanche danger, isolated pockets of MODERATE DANGER exist for human triggered avalanches 2-4' deep into old snow layering. Heightened areas of concern include steep, thin, rocky terrain on northwest to easterly facing slopes. Collapsing and cracking may or may not be present to warn you of unstable avalanche conditions. Also avoid any smooth and rounded, stiff and stubborn hard wind slabs in steep terrain.
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Special Announcements
The new UAC IOS mobile app is now available on the app store. Check out the new "My Weather" feature.

Check out the new free online avalanche course series developed by the Utah Avalanche Center. This is a great way to refresh your skills or prepare you for a Backcountry 101 or Level 1 class.
Weather and Snow
Skies are partly-becoming-mostly cloudy with temps in the upper 20s. Mercifully, the winds have died down and are generally less than 10mph from the southwest. Riding conditions in the backcountry are best described as variable. 2-3' of snow exists in the high country with about a foot at the trailheads.

We'll see a trace to two overnight into tomorrow. Winds will again be the spoiler, with the west-northwesterlies expected to increase to 35-40mph along the ridgelines. Clearing for later Wednesday into Thursday with another weak system on Friday. I know that the holidays are upon us but it's never too late to try to be good. Storms may arrive around Christmas.
Recent Avalanches
In the Primrose Cirque above Aspen Grove on Saturday, a skier and a dog took a small ride in a wind slab while walking uphill. This wind slab was 70' wide and around a foot deep. The group decided not to head up any higher due to more consequential terrain above. All observations can be found HERE.

I went to look at the conditions in the Provo mountains Sunday. We did note one large natural avalanche high along the Cascade ridgeline from one of the recent wind events to confirm evidence of old snow layering.
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Avalanche Problem #1
Persistent Weak Layer
Type
Location
Likelihood
Size
Description
In my outing into the south fork of Provo Canyon yesterday, we found a similar snowpack as that in the central Wasatch. Old weak snow from October exists in the shady terrain above about 8500', but the overall trend is toward stabilization.
Human triggered slides into this old snow layering is becoming increasingly difficult. Still, as the observation in Argenta (north side of Kessler Peak) in BCC suggests, not impossible. If not for the slope angle and the terrain features, this slope would have avalanched. Argenta often harbors shallow, weaker snow and we - as avalanche forecasters - often seek out the outliers for testing. In 2010, Birkeland, Simenhois, and Heierli presented a great study, THE EFFECT OF CHANGING SLOPE ANGLE ON EXTENDED COLUMN TEST RESULTS: CAN WE DIG PITS IN SAFER LOCATIONS? In a nutshell, they found that we don't necessarily need to "hang it out there" and dig pits in steep terrain for it to be representative of the slope. Aspect and elevation are enough. This was great confirmation that we can assume less risk in order to gather the info we want. On a side note, I know of at least two people who - when performing tests in a snowpit - triggered and were caught and carried in an avalanche. They ended up being ok, but I am still wondering how to score those test results. (cartoon from Mike Clelland of the Allen and Mike's book series - check them out)
General Announcements
This information does not apply to developed ski areas or highways where avalanche control is normally done. This forecast is from the U.S.D.A. Forest Service, which is solely responsible for its content. This forecast describes general avalanche conditions and local variations always occur.