Mt Hood

Avalanche danger will increase throughout the day at upper elevations, where fresh snow and moderate ESE winds are building wind slabs that may become large by the end of the day. Monitor the depth and consistency of new snow as you travel. If you find punchy snow or suspect wind-loading in your terrain, travel on wind-scoured slopes, or terrain less than 35 degrees to maintain a margin of safety.

Snow and Avalanche Discussion

Change is coming to the Mt. Hood region on Monday. After several weeks of very quiet weather, the Mt. Hood region is experiencing it’s first real storm since March 13th. The intervening time period has brought spring-like melt-freeze conditions to the majority of the forecast terrain on Mt. Hood as the mild temperatures and sunshine has rapidly incorporated 2-5” of convective snow that fell Wednesday through Friday. Pro observer Nick Asher traveled up to 8000 ft on the south side of Mt. Hood and found a melt-freeze throughout the terrain, softening before noon, but not producing loose wet activity. The melt-freeze crust is expected to provide a firm surface underlying the new snow that falls on Monday.

We forecast rain to fall below treeline (up to 6000-6500 ft). While the snowpack should handle the water well in most locations, keep your eyes open for soft or mushy snow deeper than your ankles. If you find these conditions, steer away from slopes steeper than 35 degrees.

The Mt. Hood Meadows base lost 22” of snow depth since March 13th, due to a combination of melt and snowpack consolidation. An NWAC pro observer reports that at elevations below 4000 ft, snow cover is disappearing quickly. Near and above treeline, shallower terrain on south-facing slopes, such as near ridgelines, is starting to lose snow as well. The mountains are still undergoing a seasonal transition, so be suspicious of sagging snow over creeks or on logs as it may well fail. Glide cracks also pose a hazard in the terrain.

March 29nd, 2019

Note added March 31st, 2019: The avalanche problems are changing only for the Mt. Hood region as a storm arrives from the south on Monday. Check the "Avalanche Forecast" tab for up-to-date information for this zone.

Peak snowpack, spring strategy, and the scale of loose wet avalanches

Peak Snowpack

Now that March is winding down, let's take have a look at the snowpack on a seasonal scale. One good question to help put things into perspective is:  “Have we hit peak snowpack depths?” This question is easily answered by, “It depends”. Have we hit peak snowpack for lowland areas? Yes, that occurred in the last month at some point. Have we hit peak snowpack depths for mountain locations at around 6,000ft? Most likely, but that could still change. You can see in the graph below that we have a range in the date of peak snowpack depth by location. This is most likely due to a variation in storm tracks, and elevation differences.  

Mount Baker, Heather Meadows (4,210ft): February 13 with 154”

Washington Pass, Base (5,450ft): February 13 with 76”

Stevens Pass, Schmidt Haus (3950ft): February 23 with 92”

Paradise at Mount Rainier National Park (5,400ft): Tied for February 20 and March 13 with 159”

Snowpack depth in inches over time from early December 2018 through March 29, 2019.

You can see that the last substantial winter storm to hit the state was in mid-March, since then we’ve been on the general decline in snowpack depths. Initially, this timeframe started with very warm temperatures and strong sun for over a week. The snowpack began to warm up, and at lower elevations, it melted. This brought on a prolonged cycle of wet loose avalanching, with many slides gouging deep, into older snow. Since then, temperatures have moderated, and the melt has slowed, but not stopped. This early-spring interlude looks to continue for the short term, but April may bring a shift in the weather pattern.

Spring Strategy

With mostly stable weather and a mostly stable snowpack, many folks have shifted their backcountry travel strategy to what may be referred to as the “Spring Diurnal Mindset”. Check the link to the paper by Roger Atkins on the most excellent “Strategic Mindset”. During a Spring Diurnal mindset, professional ski guide operations typically check to make sure an adequate overnight refreeze has occurred. Once a slope thaws, avalanche terrain is avoided on that aspect, and the group shifts to a different aspect or calls it a day. This is because the trend of avalanche danger, along with other mountain hazards (such as cornice fall) during this type of pattern tends to fluctuate. At night, the sun drops below the horizon, the air temperatures cool, and the snowpack refreezes. In the morning, the sun rises and hits the slopes, and the crust that has been thickened over a period of similar days begins to melt and become weaker. Prime recreating on sun softened slopes can occur when you find that balance of melted snow on top, but still some frozen crust underneath. The “corn harvest” occurs when you have a supportable crust beneath this sun-softened snow. When that crust is fully melted, and the snowpack underneath contains wet, saturated snow, the snowpack becomes weak and potentially dangerous. Wet loose avalanches may be initiated, along with wet slabs if there are weak layers lingering in the pack.   

The sun’s energy (shown here as Watts per meter squared) is much stronger than it was earlier in the season, as such, it’s influence on the snowpack is substantial. The increasing daily would trend look a bit more consistent if it were not for cloud cover. From the Paradise Wind Site at 5,380ft in Mount Rainier National Park.

The Scale of Loose Wet Avalanches

As mentioned, the initial pronounced warmup of the season changed our snowpack from a cold, dry, winter pack to a spring-like one. During this time (March 15-22) the mountains went through a prolonged period of wet loose avalanching. Many “gouging” wet loose avalanches were observed. These got to be large and destructive on some big terrain features. Eventually, the temperatures cooled, and luckily, most of the damage was done.

Large, gouging wet loose avalanches ran in a large south facing gully near Mount Cashmere. March 20, 2019.

Chunky, old debris from a wet loose avalanche that gouged into older snow above Eightmile Lake. This slide ran over a 1,000ft vertical and broke some small trees. March 27, 2019.

Most recently, we have been experiencing a daily refreeze of the surface, which has put a freeze (get it? hahaha) on the wet loose cycle. With this thicker and more stout surface crust, anytime we receive more than a few inches of snowfall and it lands on top, it will be time to start thinking “wet loose avalanche” all over again. The strong sun of spring won’t take long to begin changing the snow on the surface. These “superficial” wet loose avalanches tend to be fairly predictable in nature, and direct evidence such as rollerballs, moist snow surfaces, and small loose wet slides alert us to reactive conditions.

With both flavors of wet loose avalanches (gouging wet loose, and superficial wet loose) the scale of the slope is important. The larger the slope, the larger these slides may become.

Small wet loose avalanches that ran on the recently buried crust, on a fairly small slope. March 26, 2019.

Wet loose slide from the same day. A larger slope allowed a larger avalanche to run, even though it ran on top of the same crust. March 26, 2019.

The High North

It is still winter on the high elevation, north facing slopes. Here, cold, dry snow can be found. In some areas above 6,000ft faceted snow may even be found on the surface. This is something to keep in mind when this lovely spring “interlude” breaks, and the storm track inevitably shifts back to our direction.