Hatcher Pass Avalanche Center

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ARCHIVED - Forecasts expire after 24 hours.
Issued
Sat, December 11th, 2021 - 7:00AM
Expires
Sun, December 12th, 2021 - 7:00AM
Forecaster
Allie Barker
Avalanche risk The Bottom Line

It will be possible to human trigger 12 to 18″ thick persistent slabs at all elevations, on SW to NE aspects today.

It will be possible to human trigger 2 to 6″ thick wind slabs at mid and upper elevation, on W to N aspects today. Naturals are unlikely.

Winds events on 12/5-6 and 12/9 have transformed the snowpack and conditions at Hatcher Pass, scouring ridges, loading leeward aspects, and making powder hard to find.

Heads up! Winds are forecasted to increase Sunday which will increase the avalanche danger.

Sat, December 11th, 2021
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

Strong winds on 12/9 drifted snow which overloaded the persistent weak layer resulting in a number of mostly small natural persistent slab avalanche releases.

12/9 Marmot gully 1. Natural cornice fall/wind slab gouges out the facets 3200′ S aspect

12/9 Marmot South ridge. Natural avalanche, persistent slab, 3200′ S aspect

12/9 Near Marmot Mid-rib. Natural avalanche, small persistent slab, 3600′ NW aspect

12/9 Marmot, Death Gully. Natural avalanche, persistent slab, 4000′ NW

12/9 Marmot SW Face, Natural wind slab, 4500′ SE

12/8 Fishhook Creek. Human triggered slab avalanche 3000′, NE. New snow and wind blown snow have masked evidence.

 

Avalanche Problem 1
  • Persistent Slabs
    Persistent Slabs
  • Certain
    Very Likely
    Likely
    Possible
    Unlikely
    Likelihood
  • Historic (D4-5)
    Very Large (D3)
    Large (D2)
    Small (D1)
    Size
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of 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.

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

12 to 18″ thick Persistent Slabs will be POSSIBLE to HUMAN TRIGGER today on SW to NE aspects at all elevations. Naturals avalanches are unlikely.

Until this week, the snowpack at Hatcher Pass has lacked a slab. Our least favorite but most talked about problem, the persistent slab, has returned to the forecast.

Persistent slabs are sitting on weak sugary snow which encompasses the entire base of the snowpack.  Stiff snow sitting over weak snow is widespread. However the persistent slab problem is more prevalent and reactive on SW to NE aspects where winds have drifted and loaded snow.

This slab varies from 1F+hardness to 4F hardness. Hard slabs can be dangerous because they are capable of breaking above you and not just at your feet like soft slabs. Hard slabs can be stubborn to trigger, can propagate further, and can be harder to escape.

Stay out of harms way by identifying and avoiding these slabs, spacing out across the slope, and using appropriate safe zones.  Use pole tests and hand shears to help identify the persistent slab with hard snow sitting over soft snow.

Whumping, shooting cracks, and recently human triggered avalanches will be red flags for this avalanche problem.

Expect this avalanche problem to persist in the snowpack for awhile.


The video below shows the persistent slab problem at mid elevation on Friday with reactive results.

 

Avalanche Problem 2
  • 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

Winds gusting ESE 20 to 37mph for 15 hours on 12/9 formed 2 to 6″ thick wind slabs on W to N aspects at mid and upper elevation. These wind slabs will be possible to human trigger today. Naturals will be unlikely.

It will be possible for these wind slabs to step down to the persistent slab, increasing the size and consequence of the avalanche.

Wind drifted snow, smooth lens shaped features, and scalloped snow can be used to identify this avalanche problem.

Whumping and shooting cracks will be red flags for this avalanche problem.

Expect this avalanche problem to heal within 24-48 hours.

12/9 Cross Loading/ Wind loaded. Avoid these loaded zones!

12/9 Wind scoured ridgeline on Hatch

 

 

Weather
Sat, December 11th, 2021

1” of new snow accumulated overnight at Frosty Bottom (2500’) and IM snotels (3550’). Winds calmed down early yesterday morning, remaining calm overnight. Temperatures have dipped into the teens this morning, and are forecast to drop just below zero today and possibly as low as -15℉ Monday morning. A cold clearing trend is forecasted today through Monday. Winds may pick up beginning Sunday. Strong winds will have the ability to once again transport and drift snow, which will be able to overload our weak poor structure in the snowpack and increase the avalanche hazard. 


 

NWS AVG Forecast here.

NWS Rec Forecast here.

NWS point forecast here.

State Parks Snow Report and Motorized Access information here.

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