Hatcher Pass Avalanche Center

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ARCHIVED - Forecasts expire after 24 hours.
Issued
Sat, February 11th, 2023 - 7:00AM
Expires
Sun, February 12th, 2023 - 7:00AM
Forecaster
Allie Barker
Avalanche risk The Bottom Line

The avalanche danger is MODERATE for soft WIND SLABS up to 6″ thick at upper elevation, on southwest to north aspects, on slopes 35º and steeper.

The avalanche danger is MODERATE for LOOSE DRY avalanches at mid and upper elevation, on all aspects, in terrain 40º and steeper.

Natural avalanches are unlikely.

Small incremental storms will continue to bring snow to Hatcher Pass this weekend.

Despite the recent wind, great conditions can be found in protected locations, however, overcast skies and snow in the forecast will make navigation challenging this weekend.

 

Sat, February 11th, 2023
Upper Elevation
Above 3,500'
2 - Moderate
Avalanche risk
Mid Elevation
2,500'-3,500'
2 - Moderate
Avalanche risk
Low Elevation
Below 2,500'
1 - Low
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

Natural and human triggered loose dry avalanches (sluffs) were observed on 2/9 in numerous locations in steep terrain 40º and steeper.

One person was reported getting caught and carried in a sluff, pulled his airbag, and buried up to his waist.  He was reported uninjured on Thursday.

Loose dry avalanches (sluffs) in Rae Wallace on 2/9

Loose dry sluffs near Marmot lodge run on 2/9

Loose dry sluffs on Marmot below summit on 2/9

Small loose dry sluffs on Marmot, wrapping corner towards Rae Wallace on 2/9

 

Small, soft wind slabs 2-5″ thick were observed on 2/10 on SW to N aspects at upper elevation as winds picked up throughout the afternoon.

2/10 Cracking and small, soft wind slabs forming Friday afternoon on Marmot south ridge at 4000′.

 

2/10 More cracking and soft slab formation observed on Friday afternoon up to 2″ thick in this location.

Avalanche Problem 1
  • Wind Slabs
    Wind Slabs
  • 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.

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

It will be possible to human trigger soft WIND SLABS up to 6″ thick on southwest to north aspects at upper elevation on slopes 35º and steeper. Natural avalanches are unlikely.

Winds picked up around 1 pm on Friday, gusting ESE 21-26mph at 4500′ for 8 hours. Winds have started to diminish as of 6 am this morning.

Expect this avalanche hazard to be small and manageable. A ski/slope cut can be a useful tool for experienced skiers/riders for managing this shallow, soft slab avalanche problem.

Wind speeds at mid and low elevation were not able to transport snow and build winds slabs, therefore, it will be unlikely to trigger a wind slab below 3500′.

Look for hard snow sitting over weaker snow, smooth and rounded or lens shaped features.  Shooting cracks or whumping are signs of instability and indicators of this avalanche problem.

New snow expected today combined with low visibility will make finding these wind slabs a little more challenging. 

Expect the wind slab problem to improve within 24 hours after winds subside.

We always recommend using safe travel protocol in avalanche terrain:

  • SPREAD OUT when ascending.
  • Descend ONE at a time and regroup in identified safe zones.
  • Avoid riding above or near cliffs, rocks, gullies or other hazards.
  • Carry a transceiver, probe, and shovel, and know how to use them!

 

Avalanche Problem 2
  • Dry Loose
    Dry Loose
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Dry Loose
Dry Loose avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These 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.

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

It will be possible to human trigger small to large LOOSE DRY avalanches with 6 to 10 inches of low density snow in protected locations, on all aspects, at mid and upper elevation, on slopes 40° and steeper. Natural avalanches are unlikely.

In some locations, loose, low density snow is sitting on older firm surfaces and crusts, giving new snow from Feb 1-8th a smooth bed surface to slide on.

Cold temps in the teens and single digits over the the past 5 days have assisted the low density snow in the faceting process which means sluffs can run faster and potentially catch you off guard.

Triggering any loose dry avalanche has the potential to be consequential especially if caught and carried near cliffs and other hazards where being swept could compound the hazard.

Sluff management skills are recommended if skiing or riding the steeps.

Loose dry avalanches observed on 2/9 all along Rae Wallace. One rider on Thursday was caught and carried in a sluff, pulled his airbag, buried up to his waist, and was reported uninjured.

 

Weather
Sat, February 11th, 2023

2/10 Winds increased ESE 10-14mph, gusting 21-26mph for 8+ hours at 4500′.

No new snow since 2/8.


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