If you are recreating, please do so responsibly. This includes following social distancing requirements, not taking actions that risk pulling emergency service workers away from the important work they’re doing, or compromising their ability to continue that work.
To prevent spread of COVID-19, please do not travel to Flagstaff for recreation. If you are local to Flagstaff and choose to head to the backcountry, every effort should be made to avoid injuries. Now is not the time to visit a hospital which may be overwhelmed due to COVID-19. Know the conditions and know your limits!
Winter conditions returned to the Peaks in February with 45" (114 cm) of snowfall, cold temperatures, and significant wind transport of low density snow (Snow Water Equivalent of @ 3.4").
Thin coverage and rock/log hits are likely.
Natural avalanches are unlikely, but human triggered avalanches are possible, with increasing likelihood of moderate severity with added weight from wind transport and or precipitation. The weak basal facet structure of the snowpack has shown low strength and moderate to high propagation reactivity.
Currently, year to date snowfall is at 75" (190 cm) at 10,800', with a settled base depth of about 37" (94 cm) on a sheltered NW aspect. 9,500' base depth is @ 22" (56 cm).
Avalanches may be possible near and above treeline where wind slabs have developed with continued wind transport from the south (S) and southwest (SW), as well as strong north (N) winds 2-25-18, though some starting zones are more rocks than snow, especially on south aspects. Observations from the past week in the Inner Basin indicated continued wind slab deposits on a variety of aspects along ridge lines, as well as cross loading at lower elevations, increasing load on existing weak layers.
Basal faceting has been observed on generally N facing aspects near treeline, from ground level up to 30 cm (See snow pit diagrams under the 'Snowpack' tab), and has demonstrated failure and propagation on these facets, though spatially variable.
Significant cold (below freezing) temperature gradients are present in the mostly thin snowpack, exacerbating facet formation and weakening the snowpack, especially on northerly aspects.
View snow pits at snowpilot.org.
Near and Above Treeline:Above treeline wind events have loaded leeward North and South facing slopes near ridge lines in the last week, creating wind slabs that have demonstrated varying levels of stability. On Sunday, February 25, strong post storm North wind transported much of the 9% density powder snow either onto South aspects or directly into sublimation.
With similar conditions continuing, a greater likelihood of human triggered wind slabs exists, either in thin starting zones or cross loaded areas below ridge lines.
Below Treeline:With ~37" (94 cm) undisturbed settled snow depth at 10,800', NW aspect, coverage is improving but insufficient to cover many obstacles. Rocks and logs remain primary hazards. Most northerly aspects will have the best coverage with measured depths above 10,000 ft ranging from 22" - 50" (56 cm to 127 cm), while south facing slopes range from limited coverage to 28" (70 cm) in favored locations near treeline. Melt freeze crusts in the south facing snowpack may help support the weight of a skier
Watch out for small isolated slabs of new snow, wind deposits and storm accumulation perched on older layers.
Also, the snow depth is highly variable due to wind transport and sun affect, aspect dependent.
Wind slabs and/or wind loading is probable on all aspects, as winds have shifted around the compass dial repeatedly this last week.
With a forecast of possible new snow accumulation accompanied by moderate to strong winds, wind slab creation may increase potential hazard.
The thin snowpack continues to create basal facets and depth hoar, especially on northerly aspects. Wind slabs on top of these weak facets are potential areas of instability on all aspects. Be cautious of previously loaded terrain with slope angles exceeding 30 degrees, and runout zones which may hold more snow than starting zones.
Backcountry Permits are required for travel in the Kachina Peaks Wilderness and available at local USFS locations, as well as at the Agassiz Lodge on Saturday and Sunday until 11 a.m.
"Uphill travel on terrain within the Arizona Snowbowl ski area is currently unavailable due to mountain operations and construction projects."
Last updated on Thursday, March 1, 2018
Northern Arizona continues to occupy a favorable position within the western storm track, however a bit south of the core energy. Last weekend’s storm produced almost a foot of cold low density snow at treeline. On Tuesday night and Wednesday February 28th another foot plus was laid down at 10,800’. This storm also produced low density cold dendrites (stellar crystals) and was easily moved by moderate storm winds and stronger and gusty winds shifting to north and northwest as the storm passed. Above treeline snow stripping, sublimation, and some slab deposition is evident.
On the horizon, set to enter our region on Saturday night March 3th, one more storm, however this time most of the fireworks appear to be to our north and we are expecting strong winds but little snow accumulation. A warming trend and gusty winds will characterize the upcoming work week.
On Thursday evening, March 1st the Inner Basin SNOTEL site (Snowslide) reported a snow depth of 26 inches (66 cm) at 9730’, and Arizona Snowbowl reported a settled base of 41 inches (104 cm) at 10800'. So far this winter, 75 inches (190.5 cm) of snow has fallen at the mid-mountain study site. Since February 23rd, SNOTEL temperatures ranged between 3° and 40° F. For the same period the AZ Snowbowl Top Patrol Station (ASTP) temperatures ranged between –0.5° and 2 9° F.
Agassiz Peak Station 11500'
Snowslide Canyon Snotel (Inner Basin) 9730′