Avalanche forecast

Salt Lake

Utah Avalanche Center
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Out of date — this forecast expired 4 months ago. You’re viewing past conditions, not the current bulletin.

Highlights

Avalanche conditions exist!

Regular avalanche forecasts have ended. We will issue intermittent updates and publish observations through May 1st. You can submit observations and avalanches HERE, and check out the most recent observations and avalanches HERE.

During the spring, there are typically three different avalanche problems:

  • Wet Snow: Wet loose avalanches, wet slab avalanches, roof slides, and glide avalanches
  • New Snow: New storm snow instabilities; soft slab avalanches and loose dry avalanches
  • Wind Drifted Snow: Wind slabs; soft or hard drifts of wind-blown snow

Avalanche problems

  • Loose Wet

    • All elevations
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    When cold, dry snow becomes wet for the first time, it almost always means wet sluffs (loose snow that fans outward as it descends).

    Larger wet slab avalanches can happen when melt water percolates through a layered, winter snowpack for the first time especially after multiple days of warm temperatures combined with no refreeze at night.

    Glide avalanches occur regularly in spring as the entire snowpack slides slowly on the ground like a glacier until they suddenly release into a full-depth avalanche. These occur periodically on steep rock slabs and occasionally on steep grassy slopes. Notorious glide avalanche locations include Stairs Gulch or the rock slabs in Broads Fork. Avoid crossing under any slopes with cracks to the ground in the snowpack. Remember, they come down randomly, even at night.

    Warning signs may include:

    • Rollerballs (pinwheels) in new snow that is getting wet for the first time
    • Natural or human-triggered wet sluffs
    • Small sluffs fanning out into larger slides or running long distances
    • Cornices breaking off

    These signs mean it's time to head home or change to an aspect with cooler snow. Remember, even "smaller" slides can be dangerous in high-consequence terrain, such as above a terrain trap, trees, rocks, cliffs, or a long, large avalanche path.

  • Storm Slabs

    • All elevations
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    We almost always get winter-like snow storms well in the spring. Treat each storm just like you would in winter. Avalanches can occur within the new snow typically from 1) low-density layers deposited during the storm, 2) high precipitation intensity during a storm, and 3) from wind slabs created during the storm.

    It's easy to test the new snow as you travel by jumping on small test slopes to see if they avalanche or dig down with your hand to see how well the new snow is bonding. Snow can change dramatically in both space and time, so never let your guard down. Avoid any steep slope with recent wind deposits. Practice good backcountry protocol:

    • Check your gear before every tour, and make sure each person has a working transceiver, shovel, and probe before entering avalanche terrain
    • Only expose one person to a steep slope at a time
    • Never travel above other people
  • Wind Slabs

    • All elevations
    Likelihood
    Possible
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    Wind can rapidly load snow onto steep slopes, making them more prone to avalanches. Avoid slopes greater than 30° in steepness if you see signs of wind-drifted snow, such as rounded and pillowy features, and shooting cracks. In some cases, wind drifts can sound hollow like a drum.

Special Announcement

If you are looking to travel uphill at the ski areas, then check out the UAC Uphill Travel Policypage before heading out.

Recent Activity

Ski areas reported "a busy day of ski cutting" with active avalanche mitigation today...with new snow and wind slab avalanches running fast and far on the old bed surface.

In the backcountry, every single report today indicated 'very active' avalanche conditions in the higher elevation bands, with skier triggered avalanches roughly 12-18" deep, with one soft slab reportedly propagating 1000' wide in the Boulder Basin area of White Pine in LCC. (pic below). You should read their excellent write-up HERE>. Warming and greenhousing in the afternoon also allowed for easy wet loose push-a-lanches in the new snow on some steeper mid/upper elevation shady slopes. ALL of these avalanches were large enough to catch, carry, and bury you.

We will continue to post avalanches and observations. You can submit what you're seeing HERE, and check out all recent avalanches and observations HERE.

Snow and Weather

Another good storm for the Wasatch!...with more snow expected tonight and tomorrow.

As of press time (7pm Sunday evening), the Cottonwoods are up to 10-15" of heavy dense snow, made denser by afternoon greenhousing. Snow-water-equivalent numbers are up to 1.50". The PC ridgeline has received 4-8" of dense snow. The Ogden mountains have picked up 6-12"/up to 2.20" of SWE; the Provo mountains 6" and up to 1.8" of SWE. Rain/snow lines have been tethered to 7000', give or take. Winds from the west remain elevated along the more exposed ridgelines at the mid and upper elevations and wind slabs have been a problem this afternoon.

I expect we may see another couple inches Sunday night with perhaps another 4-8" of lower density snow on Monday. Winds are expected to be light to moderate from the west and southwest. "Uneventful" weather is forecast through the rest of the week with a low pressure system well to the south. Still, the weather pattern overall looks unsettled.

AVALANCHE CONDITIONS EXIST and caution should be exercised in avalanche terrain on Monday.

Click HERE to access our weather page for up-to-date weather station data to help plan your tour based on new snow, temperature, wind speed, and direction.

Our partners at the National Weather Service put out a weather discussion HERE.

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.

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