Hatcher Pass Avalanche Center

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ARCHIVED - Forecasts expire after 24 hours.
Issued
Thu, February 24th, 2022 - 7:00AM
Expires
Fri, February 25th, 2022 - 7:00AM
Forecaster
Jake Kayes
Avalanche risk The Bottom Line

Human triggered deep persistent slab avalanches are possible at all elevations and all aspects on slopes 30º and steeper. Natural avalanches are unlikely. These avalanches will be large to very large in size. 

Remotely triggering an avalanche above you or on an adjacent slope is possible. 

Avalanche danger has lowered from High to Moderate.

 

Special Announcements

Hatcher Pass Road remains closed at mile 11.

Alaska State Parks has closed East Hatcher Pass Management Area for all use at this time. See Below for Emergency Order and Map of Closed Areas.
HPAC issues avalanche forecasts for the East Hatcher Pass Management Area.
PAC is encouraging public comments on this matter. All comments should be directed to:
Stuart R Leidner
Superintendent, Mat-Su Region
Alaska State Parks
907-745-8935
stuart.leidner@alaska.gov
Thu, February 24th, 2022
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

A very large avalanche cycle occurred due to the Valentine’s Day storm. Natural avalanches occurred after the President’s Day storm but the avalanche cycle was not as significant as the Valentines Day storm. All photos are from Feb 19th

Marmot Avalanche Path’s 1,2,3 and Firn/Archangel1. All of these paths slid in the Valentines’s Day cycle.

 

Above: Map of natural avalanches that crossed the road during the Valentines Cycle.

 

Marmot 1 and 2 cross lower road

A crown can be seen on the Punk Spines.

Fishhook Road with avalanche debris.

Some interesting avalanche debris.

A D4 avalanche in the government peak bowl west of GPRA. The debris is estimated to be 30-40′ deep in places.

Natural avalanche near Lane Glacier.

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

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

The forecast area has received a large amount of snow from the Valentine’s and President’s day storms. The Valentine’s Day storm(2/14-2/19) brought 50” of snow and 8” of water to the forecast area. The President’s Day storm(2/21-2/22) brought 22” of snow and 3.5” of water. Weak layers that were formed earlier in the season are now buried under 3-4 feet of snow. The persistent slab problem has now transitioned into a deep persistent slab problem. 

Human triggered deep persistent slab avalanches up to 4′ deep, are possible at all elevations and on all aspects, on slopes that are 30º degrees or steeper. Natural avalanches are unlikely. These avalanches will be large to very large in size. Remotely triggering an avalanche above you or on an adjacent slope is possible. Deep slabs are inherently more stubborn to trigger because of the depth of the weak layer but carry significantly more consequence. Areas with a thinner snowpack will be more susceptible to human triggered avalanches. 

To identify this avalanche problem use poles/probes to identify the Dec 26th rain crust and weak sugary snow below. Formal stability tests will be unreliable due to the fact of weak layers being buried so deep in the snowpack. The layers of concern are buried deeply. This problem will feel unpredictable and give you infrequent feedback. Human triggered avalanches will be possible days or weeks after a storm.

If you choose to enter the backcountry use low risk travel techniques. Spread out when ascending slopes and descend slopes one at a time. Safe zones will be very important when traveling in the mountains. Make sure that you are regrouping in areas that are out of harm’s way. Deep persistent slab avalanches tend to travel further than anticipated and propagate across multiple terrain features..

Some of you may be wondering how we can transition from a High danger rating to Moderate in such a short time frame. In order for the avalanche danger to be at such an elevated level, there needs to be some sort of weather event adding stress or weakening the snowpack. With no weather event (snow/rain, wind or warming) adding stress, the snowpack will continue to gain stability. Most avalanches(natural or human) occur in the first 24-48hrs of a storm. After this time period the snowpack begins to adjust to the new load. While human triggered deep slab and persistent slab avalanches can still occur days and weeks after a weather event, the likelihood begins to decrease. 

 

Additional Concern
  • Wet Loose
    Wet Loose
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.
More info at Avalanche.org

With warming temperatures at lower elevations, Loose Wet avalanches will be possible on all aspects. These avalanches will be small in size. Pay attention to temperatures and snow surfaces as the day progresses.

Weather
Thu, February 24th, 2022

The Marmot weather station’s anemometer is still frozen and is not reporting wind speeds.


Valentine’s Day Storm 2/14-2/19 totals:

Independence Mine: 50” of snow and 8” of water.

Frostbite Bottom: 27” of snow and 6.1” of water.


President’s Day Storm 2/21-2/22 totals:

Independence Mine: 22” of snow and 3.5” of water

Frostbite Bottom: 17” of snow and 2.3” of water


NWS AVG Forecast here.

NWS Rec Forecast here.

NWS point forecast here.

State Parks Snow Report and Motorized Access information here.

Observations
Recent Observations for Hatcher Pass