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Forecast for the Ogden Area Mountains

Drew Hardesty
Issued by Drew Hardesty for
Sunday, March 27, 2022
I expect the avalanche danger to reach HIGH today on some slopes. Avoid being on or beneath steep terrain. Natural and human triggered avalanches are expected.
This is a classic HIGH RISK - LOW REWARD type of day in the backcountry with a lot of uncertainty on how things will play out. Which slopes will natural, which ones will not?
I'll repeat - Avoid avalanche paths, Avoid runout zones.
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Weather and Snow
Record breaking temperatures at the surface and aloft, a layered, structured snowpack...not much good can come of this. It's rare for me to say this, but based on snow, weather, and avalanche conditions, I don't recommend skiing or riding in the backcountry this weekend.
Skies are partly cloudy. The southwest winds picked up again overnight and are blowing 20-25mph with gusts to 30. Winds on Mt Ogden are blowing 35mph with gusts to 45.
Temperatures remain well above freezing with ridgetop "lows" in the mid-40s to low 50s. It's too much.
The "last best" refreeze was Tuesday night. Look below at the temperature trend for the Ben Lomond weather station at 7700'.

We'll have periods of sun with high cirrus moving through overhead at times today. Winds will blow 20-25mph from the southwest. Mountain temperatures will rise to the upper 40s up high, the low 60s down low. The Outlook: We'll see increasing clouds and southwest winds tonight into tomorrow ahead of an early week storm. Some light precipitation may begin to fall Monday night with an initial rain/snow line upwards of 9000'+. We may see 3-6" of heavy, dense snow through Wednesday.
Recent Avalanches
The ski areas noted widespread wet avalanche activity with unsupportable wet glop in uncompacted terrain.
Avalanche Problem #1
Wet Snow
I expect more dangerous avalanches today.
Overnight temps last night (this morning) are ridiculously warm and we may yet again break records for high temps today. This is only adding more melt water down into the snowpack, weakening and loosening the bonds holding the snow onto the slopes.
These are strange times - dealing with an unusually cranky snowpack for so late in the season and subjecting it to sustained, blistering heat and record-breaking temperatures. The melt-freeze cycle in general provides a stabilizing influence on the snowpack, but once you lose the "freeze" part of the cycle, frightful things begin to happen, particularly when the sun is beating down on the mountains during the day and you have a conditionally unstable, layered, "cranky" snowpack. The melt-water now starts to potentially pool along structural interfaces, dissolve the bonds holding the snow together, and, well, initiate avalanches.
BIG PICTURE: I am worried about the wet avalanche conditions this weekend. Some of the concerns are below.
  • Wet Loose avalanches are likely on all aspects and elevations and may subsequently trigger wet slabs below.
  • Wet Slab avalanches are probable on many aspects and elevations and perhaps most likely on steep northeast to southeast facing aspects. Crown depths may be 1-3' with very wide propagation.
  • Cornices are sagging and may calve off in this heat, triggering avalanches below.
Remember that wet avalanche debris sets up immediately like concrete and difficult to excavate an avalanche victim.
Travel Advice: Avoid avalanche paths; avoid runout zones.
Avalanche Problem #2
Persistent Weak Layer
You can still trigger warm and damp soft slab avalanches 1-3' deep on our Jan/Feb PWL drought layer of facets, notably on mid-to upper elevation north to northeast facing slopes. You may also trigger these from a distance or from below. Certainly the slab and weak layer is changing with the heat, but the structure is still poor and conditionally unstable.
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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.