Hatcher Pass Avalanche Center

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ARCHIVED - Forecasts expire after 24 hours.
Issued
Thu, February 15th, 2024 - 7:00AM
Expires
Fri, February 16th, 2024 - 7:00AM
Forecaster
Ryan Lewthwaite
Avalanche risk The Bottom Line

A MODERATE avalanche danger exists at all elevations.

Above 2500 feet strong winds have formed slabs of dense snow which contributed to a large natural avalanche cycle. It will be possible to trigger a wind slab avalanche on terrain steeper than 35° in the mid and upper elevations on aspects which face southwest through northeast.

At 3500 feet and below, warm temperatures without an overnight refreeze will make it possible to trigger wet loose avalanches in melting surface snow.  

Expect a mix of firm and smooth wind affected snow and moist melting snow surfaces. Avoiding these problems will take constant reassessment as you change aspect and elevation.

Thu, February 15th, 2024
Upper Elevation
Above 3,500'
2 - Moderate
Avalanche risk
Mid Elevation
2,500'-3,500'
2 - Moderate
Avalanche risk
Low Elevation
Below 2,500'
2 - Moderate
Avalanche risk
Fri, February 16th, 2024
Upper Elevation
Above 3,500'
2 - Moderate
Avalanche risk
Mid Elevation
2,500'-3,500'
2 - Moderate
Avalanche risk
Low Elevation
Below 2,500'
2 - Moderate
Avalanche risk
Fri, February 16th, 2024
Upper Elevation
Above 3,500'
2 - Moderate
Avalanche risk
Mid Elevation
2,500'-3,500'
2 - Moderate
Avalanche risk
Low Elevation
Below 2,500'
2 - Moderate
Avalanche risk
0 - No Rating
1 - Low
2 - Moderate
3 - Considerable
4 - High
5 - Extreme
Avalanche risk Avalanche risk Avalanche risk Avalanche risk Avalanche risk
Travel Advice Generally safe avalanche conditions. Watch for unstable snow on isolated terrain features. Heightened avalanche conditions on specific terrain features. Evaluate snow and terrain carefully; identify features of concern. Dangerous avalanche conditions. Careful snowpack evaluation, cautious route-finding, and conservative decision-making essential. Very dangerous avalanche conditions. Travel in avalanche terrain not recommended. Extraordinarily dangerous avalanche conditions. Avoid all avalanche terrain.
Likelihood of Avalanches Natural and human-triggered avalanches unlikely. Natural avalanches unlikely; human-triggered avalanches possible. Natural avalanches possible; human-triggered avalanches likely. Natural avalanches likely; human-triggered avalanches very likely. Natural and human-triggered avalanches certain.
Avalanche Size and Distribution Small avalanches in isolated areas or extreme terrain. Small avalanches in specific areas; or large avalanches in isolated areas. Small avalanches in many areas; or large avalanches in specific areas; or very large avalanches in isolated areas. Large avalanches in many areas; or very large avalanches in specific areas. Very large avalanches in many areas.
Recent Avalanches

With over 72 hours of moderate to strong winds and temperatures reaching into the 40°s, surface snow conditions have dramatically changed from last week. Loose dry snow has been transported around the mountains or is actively melting and becoming unconsolidated. Natural avalanches have occurred in multiple different locations and some of them have been large enough to bury a human.

~Dylan’s Molar east of Rae Wallace a large natural D2+ wind slab avalanche with multiple paths converging with debris 4-5’ deep north & northwest aspects at 4200’ on 2/13

~Hatch Peak had two large natural D2 avalanches occur on the north/northwest aspects at around 4100 feet on 2/13

~Marmot “Death Gully” natural D2 avalanche in cross-loaded terrain feature north/northeast aspect which filled in some of that terrain trap on 2/12

~Marmot “Fern Path” natural D2.5 avalanche partially crossed groomed cross country ski corridor on 2/13

~Marmot 1 & Archangel 1 natural D2 avalanches with debris in drainages on 2/13

~Martin Mine natural D2 avalanche on a north/northeast aspect and sympathetically released an avalanche on the opposing south side of the gully both exposing the ground on 2/12

~Frostbite natural D2 avalanche on prominent northwest face above Skeetawk on 2/13

Large Natural Avalanches near Dylan’s Molar East of Rae Wallace Northwest Aspect at 4200 feet 2/14/24

Natural Wind Slab Avalanche on Frostbite Northwest Aspect at 3500 feet 2/14/24

2/14 Natural Archangel 1 path from wind slab and wet loose debris SW to SE aspects 3200-4000′. Photo: Tim Escher

Two Natural Avalanches on Hatch Peak North Aspect at 4000 feet 2/14/24

Recent Conditions

Wind Scoured Surface on Marmot South Aspect at 3800 feet 2/14/24

2/14 Marmot webcam @ 4500′ on top of Rae Wallace. Winds have turned most snow surfaces into a landscape that resembles living on the moon.

Avalanche Problem 1
  • Wind Slabs
    Wind Slabs
  • Aspect/Elevation
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Wind Slabs
Wind Slab avalanches are the 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.

Aspect/Elevation of the Avalanche Problem
Specialists develop a graphic representation of the potential distribution of a particular avalanche problem across the topography. This aspect/elevation rose is used to indicate where the particular avalanche problem is thought to exist on all elevation aspects. Areas where the avalanche problem is thought to exist are colored grey, and it is less likely to be encountered in areas colored white.

Likelihood of Avalanches
Terms such as "unlikely", "likely", and "certain" are used to define the scale, with the chance of triggering or observing avalanches increasing as we move up the scale. For our purposes, "Unlikely" means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. "Certain" means that humans will be able to trigger avalanches on many slopes, and natural avalanches are expected.

Size of Avalanches
Avalanche size is defined by the largest potential avalanche, or expected range of sizes related to the problem in question. Assigned size is a qualitative estimate based on the destructive classification system and requires specialists to estimate the harm avalanches may cause to hypothetical objects located in the avalanche track (AAA 2016, CAA 2014). Under this schema, "Small" avalanches are not large enough to bury humans and are relatively harmless unless they carry people over cliffs or through trees or rocks. Moving up the scale, avalanches become "Large" enough to bury, injure, or kill people. "Very Large" avalanches may bury or destroy vehicles or houses, and "Historic" avalanches are massive events capable of altering the landscape.

Signal Word Size (D scale) Simple Descriptor
Small 1 Unlikely to bury a person
Large 2 Can bury a person
Very Large 3 Can destroy a house
Historic 4 & 5 Can destroy part or all of a village
More info at Avalanche.org

On Monday 2/12 moderate to strong south & southeast winds began to transport any available snow creating firm slabs up to 3 feet thick on leeward aspects. Most of these wind slabs can be found on slopes facing southwest through northeast. It will be possible to trigger these slabs in the mid and upper elevations on slopes steeper than 35°. Slabs are thinner and less pronounced at low elevation. Since Monday the winds have been consistently moderate to strong with extreme gusts of 68mph recorded on Marmot Peak at 4500 feet.    

Wind transported snow has the capability of loading slopes ten times faster than any storm can produce. Rapidly loading snow is a major RED FLAG and has contributed to this cycle with multiple natural avalanches occurring on a variety of different aspects. Natural wind slab avalanches up to 3 feet thick have been observed on leeward slopes and cross-loaded terrain. Some of these avalanches have propagated below ridgelines and cornices, exposing the ground. A couple of these avalanches converged in drainages and sympathetically released avalanches on adjacent slopes, making the debris in terrain traps that much deeper.

The 72 hour duration and intensity of the wind has changed the enjoyable riding conditions, leaving in its wake a lunar landscape. Raised ski tracks (anti-tracks), sastrugii (wind sculpted snow), and older avalanche debris has emerged from the snowpack as the unconsolidated snow is being eroded away by fierce winds. Below these slabs a mixture of recent soft snow or older faceted weak snow is unable to support the weight of the overlying wind slabs, helping contribute to the problem. Thickness, hardness and sensitivity of these wind slabs is highly variable and changes from one step to the next. 

With the current scenario it can be difficult to give accurate travel advice. Shooting cracks and audible collapses as you approach these slabs are indicators of the problem. No one enjoys riding pencil hard surfaces riddled with anti-tracks or watching your tips submarine below a breakable crust. Wind protected areas may be difficult to find in the Mid and Upper elevations. As the sensitivity of these slabs decreases with time and diminishing winds throughout today, sticking to simple and lower consequence terrain is the best approach. Smooth textureless slopes steeper than 35° will be more likely places to trigger an avalanche. We recommend avoiding steep wind-loaded slopes and terrain traps where the risk of and consequence of triggering an avalanche is more serious.

Avalanche Problem 2
  • Wet Loose
    Wet Loose
  • Aspect/Elevation
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Wet Loose
Wet Loose avalanches are the 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. 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.

Aspect/Elevation of the Avalanche Problem
Specialists develop a graphic representation of the potential distribution of a particular avalanche problem across the topography. This aspect/elevation rose is used to indicate where the particular avalanche problem is thought to exist on all elevation aspects. Areas where the avalanche problem is thought to exist are colored grey, and it is less likely to be encountered in areas colored white.

Likelihood of Avalanches
Terms such as "unlikely", "likely", and "certain" are used to define the scale, with the chance of triggering or observing avalanches increasing as we move up the scale. For our purposes, "Unlikely" means that few avalanches could be triggered in avalanche terrain and natural avalanches are not expected. "Certain" means that humans will be able to trigger avalanches on many slopes, and natural avalanches are expected.

Size of Avalanches
Avalanche size is defined by the largest potential avalanche, or expected range of sizes related to the problem in question. Assigned size is a qualitative estimate based on the destructive classification system and requires specialists to estimate the harm avalanches may cause to hypothetical objects located in the avalanche track (AAA 2016, CAA 2014). Under this schema, "Small" avalanches are not large enough to bury humans and are relatively harmless unless they carry people over cliffs or through trees or rocks. Moving up the scale, avalanches become "Large" enough to bury, injure, or kill people. "Very Large" avalanches may bury or destroy vehicles or houses, and "Historic" avalanches are massive events capable of altering the landscape.

Signal Word Size (D scale) Simple Descriptor
Small 1 Unlikely to bury a person
Large 2 Can bury a person
Very Large 3 Can destroy a house
Historic 4 & 5 Can destroy part or all of a village
More info at Avalanche.org

With the recent warm temperatures reaching mid 40°s Fahrenheit at 2700 feet, and lack of an overnight refreeze for 3 evenings in a row below 2700 feet, surface melting of the snow has occurred. Last night temperatures did not get below freezing up to 4500 feet at our Marmot weather station. Melting is most pronounced in the Mid to Lower elevations and is especially apparent on slopes that face south, into the sun. Yesterday at Independence Mine the temperature peaked at 41°F, although intermittent strong winds kept snow surfaces mostly dry. Rollerballs and easily formed snowballs are indicators that loose wet avalanches are possible. If temperatures continue to remain warm overnight without a drop below freezing, expect this problem to increase.

Low elevation may be the best riding conditions but expect temperature to dictate whether the surface is squishy and moist or its crusty and refrozen. The projected weather forecast does show somewhat of a decrease in temperature for the mid and upper elevations but temperatures will hover near freezing below 2500 feet.

Weather
Thu, February 15th, 2024

Strong sustained winds with extreme gusts at Marmot Weather station 4600 feet

NWS AVG Forecast here.

NWS point forecast here.

Marmot Weather Station here.

Independence Mine Snotel here.

Frostbite Bottom Snotel here.

State Parks Snow Report and Motorized Access information here.

XC trail grooming report for Mat-Su, Anchorage, and Kenai here.

Observations
Recent Observations for Hatcher Pass