We had it for a bit. We had it and now it's gone. No, I'm not referring to the regrets felt during a breakup. We had what felt like real winter for about half a week and now it's all but disappeared. In fact, it may be in the rearview for quite some time.
Weekend in Review
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| 12Z 2/22/2026 500 mb heights and temperature analysis from this past weekend. Ridge axis overlaid in red. |
The weekend warmed up nicely as a longwave ridge setup across the western U.S. There were some great bluebird conditions, and what seems like a relatively strong sun, to enjoy the fresh snow from last week's storm. It's already late February, which means the sun is much higher than what it was at the winter solstice. Daylight hours in SLC have extended from near 9 hours in late December to 11 hours at present (2/23) and the sun maxes out about 10 degrees higher in the sky. The combination of the sun and warmer temps this weekend brought hints of spring, and more "spring-like" weather is in the forecast.
The Workweek and a Bit Beyond
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| GOES-19 East from 2/23/2026 with 500 mb winds, heights, and vorticity overlaid |
The upper level ridge remains firmly centered across Utah, with high clouds streaming in over the state from the west. Mostly sunny conditions with warmer temps and high clouds are expected for Monday. Tuesday remains warm with increasing clouds and winds out of the south.
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| Timeline of northern Utah weather events 2/23-2/29/2026 |
This week we only have one storm on the docket for Utah, and it will be warmer. The upper-level ridge in place now across the western U.S. will be quite stubborn. An atmospheric river (AR) will come across the top of the ridge early to mid-week, progressing into Utah Tuesday-Wednesday (2/24-2/25/2026). As is usual with AR's, they are capricious and somewhat fitful, particularly for Utah. They can provide significant amounts of moisture or just be a tease. They can also be accompanied by warmer airmasses, which can spell heavier snow and higher snow levels. This AR looks to be sourced from subtropical origins to the southeast of Hawaii. Two lows spinning out in the Pacific will facilitate the transport of moisture into the western U.S., but the lows will remain far out to sea. This will keep the flow southwesterly to westerly along the western seaboard and conditions warm.
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| GOES-19 West True Color imagery 2/23/2026. Low pressure centers and estimated AR transport overlaid |
Flow increases out of the southwest on Tuesday, bringing some warm air advection and increased low to mid-level temperatures across Utah. AR moisture and energy begins to progress over the top of the ridge into Utah come late Tuesday into Wednesday, flattening the ridge some. Two streams of moisture will merge across Utah - one of a more southerly origin and one from a more northerly direction - and a strong jet max will slide south over the northern tier of the state. The moisture confluence/transport and jet dynamics should enhance large scale lift across the northern third of the state, producing a healthy amount of precipitation over the Wasatch Front mountains and possible the valleys. However, much of this will remain in liquid form rather than frozen. At the tail end of the storm on Wednesday, a shortwave trough will graze the state, bringing some cooler air but unfortunately nothing significant.  |
| ECMWF 00Z 2/23/2026 four-panel forecast 2/23-2/26/2026: (Top left to bottom right) 850-700 mb vertical velocity; 300 mb gph, winds, and divergence; 700 mb gph, RH, temp, and winds; MSLP, 1000-500 mb thickness, and precipitation type |
In the four panel plot above, 850-700 mb vertical velocity, 700 mb moisture, and 300 mb divergence are shown. The areas where the warmer colors in the 850-700 mb and 300 mb figures (yellow, orange, reds) overlap with 700 mb moisture (green) outline the locations of greatest forecasted lift and potential for precipitation.
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| 12Z ECMWF 2/23/2026 forecasted 700 mb temperatures (C) (2/23-2/25/2026) |
The pattern through the course of the storm will largely remain more zonal (west to east) rather than northwesterly or northerly. This means not much cold air will make it's way into Utah and snow levels will remain fairly high. 700 mb temps will oscillate around 0-+1 C late Tuesday through Wednesday morning, translating to snow levels as high as 8000-8500' at the beginning of the storm. The marginal push of cooler air late Wednesday looks to bring 700 mb temps down to around -3 to -4 C, with the rain/snow line dropping down to around 7000' (loop above). But by this time, most of the moisture will be exiting the region. Precipitation shuts down in the Wasatch by the second half of Wednesday night, with dry conditions returning Thursday morning.
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| 00Z ENS ECMWF 2/23/2026 Total snow accumulation (in) at Alta, Utah. |
Snow totals in the higher elevations will be depressed due to the warmer conditions, and the bases of most of the ski resorts will likely see rain or at least a rain/snow mix at some point during this storm. Not exactly fun. Liquid totals will range from 1-2", with total snow accumulations ranging from 6-12"+ for elevations above 7000-8000'. Snow accumulations will be heavily dependent on the oscillating rain/snow line.
Looking Ahead
A break in storm activity is expected Thursday through Friday, with milder temperatures continuing. Another shot of AR moisture and energy is possible this weekend to close out February (2/28-2/29), but once again it looks to have warmer storm characteristics. Rubbing the crystal ball, the ensemble ECMWF and GFS projects that the first week of March will be quiet with above normal temperatures. We're getting closer and closer to actual spring and winter is now slipping through our fingers, mainly in the valleys. However, big winter storms are not uncommon in March and even April, so there's still time... maybe...
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| 00Z ENS ECMWF 2/23/2026 forecasted highs and lows (F) for SLC |