The snow was quite damp below about 8,500'. Dry above 8,500' with 3 inches of dense graupel on top. In places above about 9,000' you can find a thin rain crust just beneath the graupel. In most areas it is quite thin and hard to detect, but in other places it is thicker. I'm not sure why there is such variability as rain is usually fairly evenly distributed. It could be that in some places there is a sun and wind crust as well, which makes tracking this thin crust hard. It will be interesting to see how this affects metamorphism during the coming colder weather and high pressure.
Red Flags
Wind Loading
Red Flag Comments:
No big red flags today but there was some localized wind loading along the upper elevation ridges. Winds are forecast to pick up and blow harder on Friday and Saturday from the west. So we will have to carefully watch for any recent deposit of wind drifted snow.
Primary Concern
Primary Concern:
Wind Slabs
Probability:
Moderate
Aspect:
North
Northeast
East
Southeast
South
Southwest
West
Northwest
Elevation:
High
Trend:
More Dangerous
Primary Concern Comments:
The main concern is wind loading. The preexisting snow is extremely weak, deep, faceted snow in all areas. I could see some wind loading today with the moderate winds on many of the upper elevation slopes and with the forecast of stronger winds on Friday and Saturday, we should have some dangerous wind slabs in upper elevation, wind exposed areas.
So as always, avoid any steep slope with recent wind drifts because it will almost certainly be dangerous with the stiff, heavy wind slab on top of the extremely weak, faceted snow. It won't take much.
snow_profile_location:
Observed Danger Rating:
Moderate
Forecast Danger Rating:
Considerable
2242 West North Temple | Salt Lake City, UT 84116 | (801) 524-5304 | (801) 524-6301 Fax | Advisory Hotline: (888) 999-4019
The snow was quite damp below about 8,500'. Dry above 8,500' with 3 inches of dense graupel on top. In places above about 9,000' you can find a thin rain crust just beneath the graupel. In most areas it is quite thin and hard to detect, but in other places it is thicker. I'm not sure why there is such variability as rain is usually fairly evenly distributed. It could be that in some places there is a sun and wind crust as well, which makes tracking this thin crust hard. It will be interesting to see how this affects metamorphism during the coming colder weather and high pressure.