Mt Hood

Winds were still transporting snow on Friday near 7000 ft where you might find fresh slabs. Lower down the mountain, large wind slabs linger near and above treeline in some locations and might be triggered on unsupported slopes or convex roll-overs. Loose wet and loose dry point releases will need to be managed on steeper slopes where a small slide may be consequential.

Two recent observations give us confidence that the deep slab is healing sufficiently to remove it from the problem list. On Friday, NWAC Pro Observer Nick Asher traveled in the Newton drainage and dug at 5800 ft on a NE aspect. He found the early February crust down 5-8 ft with connected rounds replacing facets under a very supportable 5-10 cm crust. On Thursday, Mt. Hood Meadows Ski Patrol dug to the same crust on a protected NE aspect in the very narrow elev band, 5300-6000, where the facets had previously been prominent. The facets were also turning to rounds. Given no reported activity for 2 weeks and a stabilizing snow structure in this region of higher concern, we have removed the Deep Persistent Slab as a problem.

Winds have decreased following several periods of moderate to strong generally NE winds over the last 5 days. Winds freshened Tuesday, strong enough to continue transporting snow and building new fresh wind slabs. A previous round of fresh snow and strong NE winds Monday formed wind slabs on atypical aspects.

Snow storms since last Friday night brought 2-3 ft of new snow to the Mt. Hood area. This created ample snow available for transport and excellent near and above treeline, generally right-side up snow in wind-sheltered locations. A professional observation from the bluegrass ridge area found that wind slabs were not impacting the terrain below 5500 ft. 

Keep in mind that with all the recent snow, loose avalanches will be possible on any aspect. Notably, south-facing aspects may produce roller-balls and small loose wet avalanches during periods of intense sunshine. Faceting upper snowpacks on northerly aspects may run farther than you expect on steeper slopes.

March 1, 2019

Here we are at the beginning of March. The days are noticeably longer, the sun feels warmer, but the winter is far from over. This may be a good time to take stock of February’s events, where we are now, and what we might expect in the future.

A February to Remember

Many longtime Cascade travelers continue to remark about the long span of high-quality travel conditions in February. Indeed, we’ve experienced three weeks of very cold and snowy conditions. Backcountry travelers frequently reported, “best conditions in years”. February also saw a few rounds of natural and human triggered avalanches. These avalanches were different from our more frequent Cascade storm slabs; here today and gone tomorrow. Most avalanches failed on buried weak persistent layers. As such, most zones spent much of February with Persistent or Deep Persistent Slabs in their forecasts.

Natural avalanche in Icicle Creek Feb 13, 2019. Photo: Matt Primomo

With the notable absence of high elevation rain events, snowpacks around the northwest grew remarkably. On the west slope, most weather stations added 2-4 ft of snow depth. East-side locations added 1-2 ft. Mt Hood locations added 4-5 ft. Even with these impressive snowpack growths, many Cascade Snotel sites are still recording below average snow depths for the winter.  

During most of February, snow conditions were soft and powdery making for fun recreating in many areas. Photo Matt Primomo.

Where We Are Now

Lack of avalanche activity on the layer of buried facets from Feb 8 allows us to gain confidence in many areas. In some areas, snowpack tests are showing less than sudden results. These two pieces combined have allowed us to drop persistent slabs from some forecasts and shift others to “unlikely.” The exception is the East Cascades where a shallow snowpack has preserved buried facets, and persistent slabs will remain possible through the weekend. So, we’re out to the woods, right? Well, maybe. The same cold and stormy weather that brought us excellent snow quality, also allowed us to bury new weak layers. So far we haven’t confirmed any avalanches on these shallow weak layers, but they have our attention and we’re tracking them.

Recently our attention shifted to the upper snowpack. Recent avalanche problems have largely focussed on wind transported snow. Several wind events from various directions placed wind slabs on a variety of aspect. With the colder than normal temperatures, wind slabs may not heal as quickly as normal.

A small natural wind slab avalanche in the Crystal Mt backcountry. Photo; Dallas Glas

What Might We Expect

As we move into March, it’s anyone’s guess what specific weather patterns lay in store of us. However, there are two items that stick out in our minds.

• The strength of the March sun: You can already feel it just walking around town. As the sun creeps higher into the sky and the days grow longer, the sun can have a greater impact on the snow surface. When the sun comes out, expect things to change quickly. You may see slab avalanches become easier to trigger, natural loose avalanches originating from sunny slopes, or surface snow become thick and heavy. Remember, the sun frequently brings change.

• High elevation travel: Frequently March begins to usher in a period where we push higher and deeper into the mountains. Remember, we don’t have as much information about these far-flung locations. If you use the longer days of March to travel to bigger objectives, keep your eyes open. When observations don’t line-up with the avalanche advisory, you may be experiencing a different snowpack. It’s times like these we need to stop and reevaluate.

Mt Baker on a nice day in early February. Photo: Lee Lazzara

February was amazing! but March is here… there’s still plenty of winter left. Stay safe out there.