We have a decent setup for snow on the way, one that will extend the Nordic season at Mountain Dell and maybe even provide a proper deep powder day at Alta.
The GFS large-scale forecast of 500-mb geopotential height (black contours), precipitable water (color contours)m and 6-hour accumulated precipitation (color fill) for 0000 UTC 9 March (5 PM MST this afternoon) is below. It's actually not a hell of a lot different than we've seen quite a bit over the past two months. There is a ridge off the Pacific coast with a trough dropping down out of Canada.
However, there are a few favorable wrinkles this time. First, there is a plume of moisture associated with a decaying atmospheric river remnant that has snuck under the ridge and is extending into the Pacific Northwest ahead of the approaching trough. Thus, the system is not as moisture starved as many of the recent troughs. Second, the pattern is shifted a bit farther upstream, so instead of sliding into Colorado, this trough will extend far enough west to give us some action (and cold air).
The GFS time-height section for Salt Lake City shows this is a 3-part storm. It begins with the prefrontal stage, which is already bringing a little light snow to the high elevations this morning and will continue to this evening. I expect accumulations during this period to be light, perhaps adding up to 1-3 inches by 5 PM this afternoon at Alta Collins.
This evening and tonight, we have a low-level frontal passage, with the front complex in structure. During this period, snowfall rates will increase. For example, from 5 PM tonight through 5 AM tomorrow morning, the GFS generates about 0.5 inches of water and 8 inches of snow at Alta Collins.
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