Watch for the spring sun effects on the shallow new snow that accumulated on Mt Hood, especially in areas that wind may have drifted more snow. As we continue to transition to spring, pay attention to opening creeks and gulleys, glide cracks and softening cornices.
Only 2-3 inches of new snow accumulated on Mt Hood making any possible Loose-Wet avalanches generally small. However, even small slides can be dangerous if they carry you into or over a trap, such as gullies, trees, or cliffs. Watch if the wet snow is becoming greater than boot top or in areas where wind may have drifted deeper snow.
Snow and Avalanche Discussion
The front Monday night and early Tuesday morning only deposited shallow amounts of a few inches of new snow at cooling temperatures. Overall, the cooling will help strengthen the upper snowpack following a week of very warm weather.
Watch for shallow drifted snow at the highest elevations, mainly near ridges and avoid steep slopes greater than 35 degrees if you see evidence of wind drifted snow.
The new snow should be shallow enough that any Loose-Wet avalanches should be small. However, if surface snow is getting greater than boot top, you could trigger a larger wet snow avalanche.
The mountains are still experiencing their spring transition. As a result, you may find a wide variety of snow surfaces, including breakable crust, firm icy surfaces, and wet heavy snow. During this transition remember to keep a lookout for potential springtime hazards such as opening creeks and glide cracks. Use caution if you travel near these features.
March 22nd, 2019
Enter Spring
If you’ve been in the snow recently, the wintery conditions of early March may seem worlds away. You may be in for a surprise if it’s been a while since you were in the mountains. The weather has taken a turn towards spring in the last couple weeks and the Cascade snowpack the has undergone major changes. Unseasonably warm temperatures and strong sun followed a month-and-a-half of cold, winter storms. Mid-elevation weather stations stayed above freezing from March 15th-22nd with high temperatures reaching the upper 50’s to low 60’s. For an in-depth survey of the regional snowpack, we’ll divide the terrain up by aspect and elevation.
A graph showing temperatures between 4,000-5,000ft around the Cascades from the 16th-21st.
Aspects
Northerlies
Along with the warm temperatures, the spring sun has played a major role in warming snow surfaces. The result is a snowpack that varies by aspect. In most regions, shaded and northerly slopes remain relatively unchanged. Aside from some settlement and firmer or moist surfaces, the snow on north aspects is almost entirely dry. Even some low elevation north slopes are still holding snow.
Sunny slopes
The snowpack on east through south through west aspects is a different story. The strong March sun melted snow surfaces and drove melt-water into the snowpack. This is most dramatic on steep (over 35 degrees) southeast through southwest slopes below 5,000ft. In some areas, you can find meltwater up to 3 feet below the snow surface with drainage channels well established. Between this warm period and rain events in the first half of the winter, the entire snowpack has transformed to melt forms. An important point to note is that as of the 22nd, these solar aspects remain unfrozen and weak. Cooler weather ahead may help strengthen moist to wet layers.
A glide avalanche (D2) released from a rock slab late on the 20th. Lichtenberg Mtn, 5,100ft, SE aspect. Other glide avalanches occurred on the 20th at Snoqualmie Pass and in Tumwater Canyon. Photo: Josh Hirshberg
Elevation
Low elevations
As you travel from low valleys to higher peaks, you’ll notice a major difference in the snowpack based on elevation. With all the low-elevation snow this winter, there are still some cold, shaded slopes holding pockets of snow down to 1,000ft, especially east of the Cascade Crest. However, most slopes below 3,000ft have lost much of their snow cover. Many low elevation, sun-exposed slopes are bare, especially in areas that previously held less than 3 feet of snow. The low elevation snowpack is no longer substantial enough to allow for easy travel over snow or widespread avalanches.
Loose wet avalanches on the south side of Table Mtn, near Mt Baker. 3/17. Photo: Pete Durr
Mid-elevations
At mid-elevations, around 3,000-5,000ft, the snowpack is still deep and layered. Many slopes at this elevation band near and west of the Cascade Crest are holding 6-10 feet of snow. This is also where you’ll find the most dramatic variation in the snowpack based on aspect.
High-elevations
Above 5,000ft you’ll encounter a snowpack similar to what you may have found around the 1st of March. Upper elevations have stayed mostly dry. The most sun-exposed slopes have surface crusts but have not seen much water or change to melt forms below the surface.
