As of midday on Sunday January 22 storm totals had exceeded those forecasted for high elevations. By that time, Arizona Snowbowl had received 53 inches in 48 hours, with a snow depth of 90 inches at 10,800’. On Sunday, Snowslide SNOTEL, site at 9730’ in the Inner Basin, reported 81 inches (settling to 78 inches) with an accumulation of about 24 inches for the first two of three storms. Three inches of snow water equivalent (SWE) had loaded a poorly structured snowpack.
On Saturday, explosive mitigation instigated by the Snowbowl ski patrol produced a large avalanche from near the false summit of Agassiz Peak. This slide ran nearly 800’ to the radar sign on the ski area. It had a crown thickness of 2 to 4’, and was initiated by only 2 pounds of explosive. This indicates the potential magnitude of natural and skier trigger avalanches.
Arizona Snowbowl uphill access is closed until further notice.
Avalanche Danger: Snowpack stability will continue to be precarious for at least the next 48 hours.
Backcountry travelers need to be patient and allow new snow to bond with old and gain strength. Travel in avalanche terrain is NOT recommended for the next 24 hours after the cessation of precipitation. Instabilities could remain tenuous for an extended period of time. Further snow pit investigations later next week will inform us about rates of stabilization. Stay tuned and share your own observations and snow pit results.
As of Sunday morning total snowfall for the season at 10,800’ was 194 inches. This is 3/4 of our average total annual snowfall; pretty remarkable for the third week in January and another 2 feet forecasted for the third storm.
From Arizona Snowbowl: Spur Catwalk is closed due to avalanche danger. Please access Bowl Side trails via Midway Catwalk. Upper Bowl will be closed likely through Tuesday. Avalanche control work is in progress and Uphill Access is closed until further notice. This will likely be in effect through Tuesday for avalanche control work.
Near and Above TreelineVery dangerous avalanche conditions. Travel in (or near) avalanche terrain NOT recommended.
Below TreelinePow riding in the trees is all time right now. Keep your slope angles below 30° and watch for steep isolated terrain traps in gullys. Tree well hazards may be an issue in our deeping snowpack. More discussion in the last summary update.
New storm snow will need time to bond with the old snowpack. This generally happens within 24-48 hours after the end of precipitation. Storm slab avalanche hazards will continue into midweek and possibly beyond. Forecasted cold temperatures will prolong bonding of storm snow with layers below.
Optimum wind speeds for the transport of snow are currently in progress, and there is plenty of snow available to move. Higher velocity winds are also expected. Wind Slab avalanche hazards will continue into midweek and possibly beyond. Forecasted cold temperatures will prolong bonding of storm snow with layers below.
Avalanches may step down onto persistent weak layers deeper in the snowpack increasing the potential mass moving downslope. Discussed more in the last summary update.
Inner Basin surface hoar, January 18, 2017. Steep slopes with surface hoar buried by new snow is a deadly combination. Photo by Derik Spice.
Travelers are advised to exercise caution and make slope specific evaluations. As always, please treat this summary with appropriately guarded skepticism, make your own assessments, and contribute to our body of knowledge by reporting your observations.
Want to learn more safe backcountry habits? KPAC offers level I and II avalanche courses. They are filling up fast!!!
During winter, backcountry permits are required to access the Kachina Peaks Wilderness. More info
Note: Uphill access has opened at Arizona Snowbowl. It may be restricted or closed due to heavy snow and avalanche danger. Access to the Humphreys Summit trailhead is always available from the lower lots of the ski area, below the gate. Travel safe! arizonasnowbowl.com/safety
Last updated on Friday, January 20, 2017.
As KNAU’s Gillian Ferris says, "a winter storm trifecta" is currently impacting our region, as well as, large portions of western United States. These storms will bring the most intense winter precipitation we have had this season. Snowfall total could potentially exceed 24 inches and load the old snowpack with 2-3 inches of snow water equivalent (SWE).
The first pulse was a short wave trough, starting on Thursday and was forecasted to lay down less than a foot at higher elevation. Snow level started at 6000 feet and dropped to 5000 feet by Thursday night. Snowfall will taper off on Friday morning.
A second pulse arrives on Friday evening and lasts through Saturday morning. This slightly longer wave trough will have the greatest precipitation potential. We anticipate heavy snowfall with accumulations in the 1 to 1.5 foot range above 10000 ft.
A fast moving short wave ridge will create another brief break until a third colder pulse arrives on Sunday night. Atmospheric instability is expected to last into midweek with lingering snow showers. Snowline will drop to 4500 feet, with breezy winds out of the southwest lingering. Subfreezing maximum temperatures and moderate winds will prevail for the first half of the workweek above 7000 ft.
Station Information: On the morning of Friday January 20th the Inner Basin SNOTEL site (Snowslide) reported a snow depth of 68 inches (173 cm) at 9700 ft, and Arizona Snowbowl reported 79 inches (201 cm) at 10800 ft. These values are expected to increase dramatically as heavy precipitation continues periodically for the next several days. Since January 14 the SNOTEL temperatures ranged between 11 and 35°F and Agassiz station between 12 and 25°F.
The avalanche problem/character describes part of the current avalanche danger. However because we only realease a summary once a week, the current avalanche problem will likely change.
Understanding avalanche problems is essential, because it allows you to determine your approach and strategies to risk treatment. Below are brief descriptions of avalanche problems/characters, and links to detailed information on the problem, formation, patterns, recognition, and avoidance strategies.
Avalanche Problems Explained Also see the North American Danger Scale.
Release of dry unconsolidated snow. These avalanches typically occur within layers of soft snow near the surface of the snowpack. Loose-dry avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs. Loose-dry avalanches can trigger slab avalanches that break into deeper snow layers.
Loose Dry avalanches are usually relatively harmless to people. They can be hazardous if you are caught and carried into or over a terrain trap (e.g. gully, rocks, dense timber, cliff, crevasse) or down a long slope. Avoid traveling in or above terrain traps when Loose Dry avalanches are likely.
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.
Release of a cohesive layer of snow (a slab) formed by the wind.
Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side.
Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard.
Wind 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.
Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features.
They can be avoided by sticking to sheltered or wind-scoured areas.
Release of a cohesive layer of soft to hard snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow.
Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
The best ways to manage the risk from Persistent Slabs is to make conservative terrain choices.
They can be triggered by light loads and weeks after the last storm.
The slabs often propagate in surprising and unpredictable ways.
This makes this problem difficult to predict and manage and requires a wide safety buffer to handle the uncertainty.
Deep Persistent Slab
Release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer, deep in the snowpack or near the ground.
The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
They commonly develop when Persistent Slabs become more deeply buried over time.
Deep Persistent Slabs are destructive and deadly events that can take months to stabilize.
You can trigger them from well down in the avalanche path, and after dozens of tracks have crossed the slope.
Release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers.
Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. They generally move slowly, but can contain enough mass to cause significant damage to trees, cars or buildings. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
Travel when the snow surface is colder and stronger. Plan your trips to avoid crossing on or under very steep slopes in the afternoon. Move to colder, shadier slopes once the snow surface turns slushly. Avoid steep, sunlit slopes above terrain traps, cliffs areas and long sustained steep pitches.
Release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very destructive.
Avoid terrain where and when you suspect Wet Slab avalanche activity. Give yourself a wide safety buffer to handle the uncertainty.
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side.
Cornices range in size from small wind lips of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.
Cornices can never be trusted and avoiding them is necessary for safe backcountry travel. Stay well back from ridge line areas with cornices. They often overhang the ridge edge can be triggered remotely. Avoid areas underneath cornices. Even small Cornice Fall can trigger a larger avalanche and large Cornice Fall can easily crush a human. Periods of significant temperature warm-up are times to be particularly aware.
Large cornices are generally rare in Arizona, but they have been observed during very snowy winters.
Release of the entire snow cover as a result of gliding over the ground. Glide avalanches can be composed of wet, moist, or almost entirely dry snow. They typically occur in very specific paths, where the slope is steep enough and the ground surface is relatively smooth. The are often proceeded by full depth cracks (glide cracks), though the time between the appearance of a crack and an avalanche can vary between seconds and months. Glide avalanches are unlikely to be triggered by a person, are nearly impossible to forecast, and thus pose a hazard that is extremely difficult to manage.
Predicting the release of Glide Avalanches is very challenging. Because Glide Avalanches only occur on very specific slopes, safe travel relies on identifying and avoiding those slopes. Glide cracks are a significant indicator, as are recent Glide Avalanches.
Glide avalanches are very uncommon in Arizona.
Snowpack Summary Disclaimer
The summaries on this site were written by Kachina Peaks Avalanche Center Board Members. They are based on a broad spectrum of data collected from weather stations, National Weather Service point forecasts and field observation by qualified individuals.
The summaries are not intended to substitute for good knowledge and decision making skills in avalanche terrain. If you have any doubt of stable conditions, please stay away from avalanche terrain. You can usually find good places to go that are not prone to avalanches, such as on low angle slopes away from avalanche run-out zones. If you have any questions about where to find such places, you should consider further avalanche educational opportunities, such as those listed on our education page.
Snowpack Summary – Format and Limitations Statement
Starting in 2012 Kachina Peaks Avalanche Center (KPAC) has publish a weekly Snowpack Summary on our website.
These summaries are currently issued on Friday afternoons. On occasion, we will give storm updates or warnings of rapidly increasing avalanche hazard at more frequent intervals.
Our objective is to reach weekend recreationist, informing this user group of prevailing conditions, but particularly warning of avalanche hazards whenever they are present.
Many people have asked us why we use the format we do, but do not include a danger rating or a hazard/stability rose as many other avalanche centers do around the west.
The National Avalanche Center (NAC) advises small operations like KPAC, who do not issue daily bulletins to not use danger ratings in our snowpack summaries due to the regular but intermittent nature of their field observations and the length of time between issuance of snowpack summaries.
A primary concern is for how conditions can change in the time between publications, potentially giving the public misleading information. At this point, we simply do not have resources to monitor the snowpack at the level necessary to accurately produce more frequent bulletins.
While we understand the benefits of a danger rating using the North American Danger Scale, we also feel that our format encourages people to dig in a little deeper, and spend some time reading what our forecasters are saying. Although the area that we forecast is relatively small, the variability has proven quite large.
Inner Basin conditions are often surprisingly different from those on the more wind-affected western side on the Peaks.
We hope the information that we provide in summaries helps give you a good overview of what is going on out there, and what avalanche problems you should be attentive to, but if there is any uncertainty, then we encourage you to ask questions via Facebook or email@example.com.