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This morning, under broken skies trailhead temperatures are in the mid-20s °F, while the highest peaks are in the mid teens °F. Winds have picked up since yesterday, blowing from the west, gusting to the 30s MPH. There was another trace to 3" of snow overnight. This storm has stealthily added a decent amount of water to some locations, bringing close to 25" of new snow to the Ogden area mountains in areas.
Today, expect lingering lake-effect precipitation in northern Utah to fade by morning due to incoming high pressure, resulting in warming and drying conditions. The day will start mostly sunny but become mostly cloudy later. Temperatures will range from 34-37°F with no snow accumulation expected. Winds will be moderate, with gusts up to 20-25 MPH at mid-elevation and up to 35 MPH at upper-most elevations.
Looking ahead, after a brief break today, a strong cold front will move across northern Utah on Thursday, slowing over central or southern Utah by Thursday night or Friday morning. It will weaken and return northward on Friday, with more precipitation likely through the weekend.
Read the updated forecast discussion from our partners at the National Weather Service
HERE.
No new avalanches were reported in the Ogden area mountains yesterday.
South of Ogden, in the Central Cottonwoods, reports came in of soft slab avalanches up to 2 feet deep in
Conehead, Benson and Hedges, the
Brighton Perimeter,
Argenta, and
Little Superior Bowl. Among these, the avalanche that particularly caught my attention occurred in Little Superior Bowl. Although details are limited, it was reported as being 2 feet deep and 400 feet wide. This incident more closely resembles the avalanche in Silver Fork from Monday, which I went and checked out yesterday.
Both of these avalanches stand out for their considerable depth compared to other reported avalanches over the last two days, displaying more slab-like characteristics.
Avalanche Heat map from the past 5 days for the Salt Lake, Provo, and Ogden area mountains.
Read all the observations
HERE.