Northwest Avalanche Center NWAC, Northwest Avalanche Center

Cascades - West Avalanche Forecast

Jan 9th, 2020 10:20AM

The alpine rating is high, the treeline rating is considerable, and the below treeline rating is considerable. Known problems include Storm Slabs.

Expect conditions to become more dangerous throughout the day Friday as heavy snowfall and wind load lower density snow layers in the West-Central zone. Choose travel plans with plenty of options to navigate areas where avalanches may start, run, and stop. As snow accumulates, you could trigger an avalanche on any slope greater than 35 degrees.

Summary

Discussion

We received information late this evening of a human triggered cornice avalanche on an east gully of False Herman in the Baker backcountry. Two people were caught and carried in the event. One individual was carried approximately 200'. No major injuries were reported. The large cornice block triggered a small wind slab on the steep slope below.

Avalanche danger will increase during the day Friday due to a significant winter storm. At upper elevations, you could encounter very dangerous conditions with large natural avalanches occurring. Don’t let yourself get caught in complex terrain as conditions change. Choose routes with plenty of options to adapt to changing conditions and avoid avalanche slopes. Small changes in timing of the storm could greatly impact the avalanche hazard. We expect danger to peak during the afternoon hours with the highest precipitation rates and winds. 

Observations from Thursday near Church Lake (in the West North zone) indicate that most avalanche concerns going forward should be limited to the new snow and how it bonds to the current snow surface. At 6000 ft, NWAC staff observed nearly 2’ of settled snow over a pronounced crust buried on Tuesday. Similar conditions may be found in the West Central zone, with decreasing snow depth at lower elevations.

Snowpack Discussion

January 9th, 2020 (The regional synopsis is updated every Thursday @ 6 pm)

 

As we said Happy New Year and rang in 2020, snow was turning to rain at many trailheads and lower elevation Passes, not exactly the fresh start winter recreationalists had in mind. The snowpack was already looking a little thin throughout the region, especially at lower elevations. Low snow in places like Snoqualmie Pass made backcountry travel difficult and hazardous.  NWAC’s snow depth climatology report was showing snow depths 25-64% of normal to kick off the start of 2020.

Things can change quickly in the Pacific Northwest and they did as we entered an extended storm cycle between January 2nd to January 8th. Strong winds, fluctuating temperatures, and heavy precipitation offered few breaks in the weather over this period limiting observations and hampering travel. Despite periods of rain at lower elevations, most areas saw several feet of new snow with big jumps in total snow depths as a westerly storm track strongly favored the West Slopes of the Cascades and the Olympics for the highest precipitation totals.

 

Location

Total Snow Depth (in) 1/2/20

Total Snow Depth (in) 1/8/20

Hurricane Ridge

31

51

Heather Meadows Mt Baker

55

95

Washington Pass

49

74

Stevens Pass

41

63

Snoqualmie Pass

22

33

Alpental mid-mountain

44

63

Crystal Mt Green Valley

40

66

Paradise Mt Rainier

54

105

White Pass Upper

43

69

Timberline

36

57

Mt Hood Meadows

36

53

 

We may have started with a shallow snowpack, but most locations increased their snowpack by 70% or more over this storm cycle!

During this extended and impressive storm cycle that included backcountry avalanche warnings, natural avalanches were reported in many areas Jan 6th-7th.

The Stevens Pass area was especially active over the period with over 100(!) avalanche observations made on the 6th and 7th. Professionals reported numerous avalanches in places that they hadn't previously observed avalanches and some paths avalanched multiple times in a 24 hour period. Observers reported a few very large (size D2.5-3) avalanches, originating at upper elevations with deeper crowns that likely formed from wind drifting. Topping off an active couple of days, warming temperatures lead to a widespread loose wet avalanche cycle.

The southern Washington Cascades, the Wentachee Mountains and Mt. Hood either saw less precipitation, warmer temperatures leading to more rain than snow, or some combination of the two and ended up with relatively less active avalanche conditions than areas further north. 

A large natural avalanche on Rock Mountain near Berne along Hwy 2 east of Stevens Pass that released Jan 6th or 7th. Photo: Josh Hirshberg 1/7/20

Many small storm slabs released in the Crystal backcountry 1/6-1/7. Pinwheels in the photo suggest loose wet avalanche activity occurred when temperatures rose above freezing and snow turned to rain.

Another active and colder weather pattern is on it’s way. Enjoy yourself out there and be sure to check the forecast before heading out. Remember, NWAC is a community-supported avalanche center and when you submit an observation you make the forecast better!

-Peter Moore

It’s getting deeper! Photo: Jeremy Allyn

Problems

Storm Slabs

An icon showing Storm Slabs

Likelihood

very likely

Expected Size

1 - 1

Potential avalanches will become larger and more difficult to manage as the day progresses. Steer around any slope greater than 35 degrees when you encounter signs that a slab formed in the new snow. Periods of intense precipitation, shooting cracks, wind drifts, and strong snow over weak snow are clues storm slabs may be present.  

With such cold temperatures, storm slabs are not a given. You could encounter loose surface snow conditions. If you don’t find a slab, anticipate loose dry avalanches. Even though these sluffs are often small, they may entrain snow and run long distances in larger terrain. With changing conditions, loose snow in the morning could become a slab in the afternoon.

Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

 

You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.

 

Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.

Aspects:

All aspects.

Elevations:

All elevations.

Valid until: Jan 10th, 2020 10:20AM