Forecast for the Abajos Area Mountains

Eric Trenbeath
Issued by Eric Trenbeath on
Thursday morning, April 1, 2021
The avalanche danger is generally LOW. Isolated areas that contain steep, wind-drifted slopes at upper elevations that face N-NE could produce small avalanches in extreme terrain. As the day heats up be alert to signs of loose wet instability such as rollerballs, pinwheels, and sloppy wet snow on sun-exposed slopes. Stay off of and out from under steep slopes when these signs are present.
Low
Moderate
Considerable
High
Extreme
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Weather and Snow
Snow totals at Buckboard Flat (8924')
Snow totals at Camp Jackson (8858')
Snowpack Discussion
Warm temps and a strong March sun have rapidly settled last week's snow. Most aspects and elevations contain a 2-4 cm melt-freeze crust, and the snowpack has gained strength through time and warm temperatures. In isolated areas, weak, sugary, faceted snow still exists near the ground at the highest elevations on NW-N-E aspects. The most suspect areas are less than 5' deep and contain wind-drifted snow on top of the deeply-buried persistent weak layer. Slopes with steep convexities and rocky, more radical terrain are where you are most likely to trigger an avalanche failing on weak, faceted snow.
As the day heats up be alert to signs of loose wet instability such as rollerballs, pinwheels, and sloppy wet snow on sun-exposed slopes. Stay off of and out from under steep slopes when these signs are present.
Additional Information
Information on outdoor recreation - The State of Utah created this webpage with information about recreating on both state and federal public lands during the current health crisis.

New to the backcountry (including riding at closed resorts) - Watch the award-winning, 15 minute Know Before You Go video, or take the 5-part, free online-learning series.
General Announcements
This forecast is from the U.S. Forest Service, which is solely responsible for its content. This forecast describes general avalanche conditions and local variations always occur.