Hatcher Pass Avalanche Center

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ARCHIVED - Forecasts expire after 24 hours.
Issued
Sat, April 6th, 2024 - 7:00AM
Expires
Sun, April 7th, 2024 - 7:00AM
Forecaster
Allie Barker
Avalanche risk The Bottom Line

The avalanche danger is MODERATE for PERSISTENT SLAB and DRY LOOSE at all elevations.

30+ inches of new snow over the past week has shifted spring back to winter, brought the return of a persistent slab problem and finally surpassed the 5 foot mark on the Marmot lodge snowstake.

Remotely triggering a persistent slab up to 2+ feet thick is possible in isolated locations.

With uncertainty around the distribution and reactivity of this problem, evaluate snow and terrain carefully to identify features of concern.

Sat, April 6th, 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
Sun, April 7th, 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
Sun, April 7th, 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

8″ of new snow with 0.8″SWE @Frostbite at 2700′ and 10″ of new snow with 1″ SWE@IM at 3550′ were reported in the most recent April 4th storm. These totals finally surpassed the 5′ mark for snowpack height on the Marmot lodge snowstake! Due to the mostly right-side-up snowfall combined with light winds, we observed few recent avalanches in the field on Friday. One large persistent slab was observed up the Valley of Sin on the Ripper’s Delight on a NW aspect at 4200′ that occurred on 4/4. This avalanche likely failed on weak sugary snow sitting on a firm and smooth bed surface (as seen in photo below). Several small dry loose sluffs were observed on Friday. One human triggered persistent slab was triggered on the NW aspect of lower Microdot at 4000′. This avalanche sympathetically triggered two other slab avalanches (see photo under problem 1). 

4/4 Natural avalanche on Ripper’s Delight up the Valley of Sin NW 4200′

 

4/5 Recent small dry loose avalanches on The Knob above Goldmint parking lot. A few appear to be dry loose that transition at the bottom into wet loose. W 2400′

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

Persistent slabs 8-30″ thick will be possible to human trigger on all aspects, at all elevation, on slopes 30º and steeper.  Over 30″ of new snow has been recorded from the last two storms on 3/30-31 and 4/4.  Possible locations to trigger a persistent slab include any aspect where more cohesive slabs are sitting over weak sugary snow on firm crusts.  The good news is the continuity of the weak layer does not exist everywhere so finding a slab/weak layer combo will be challenging and less likely. The bad news is if you do find a location where this recipe exists, triggering a large avalanche will be possible.  Shallower spots in the snowpack or areas previously scoured down to old melt freeze crusts by the wind prior to the last two storms will be more likely locations to trigger a slab.

Remotely triggered avalanches will be possible from below, above, or adjacent to slopes.  This type of avalanche problem often gives unreliable feedback.  Cracking and whumping may or may not occur prior to triggering an avalanche. Pole/probe tests and formal stability tests will help you identify stiffer snow over weaker snow and where this problem exists.

Three remotely triggered avalanches occurred on 4/1 and 4/2 followed by another storm that deposited 10″ on 4/4.  On 4/5 a large human triggered slab avalanche occurred on lower Microdot that sympathetically triggered two other avalanches (photo below). Obs here. The slab thickness will vary depending on aspect and elevation. Expect thicker slabs up to 30″ at upper elevation or on leeward (northerly) aspects and thinner slabs 4-8″ thick at low elevation or on windward (southerly) aspects.

4/5 Human triggered persistent slab that sympathetically triggered two other slab avalanches. No one was caught and carried. Lower Microdot, WNW 4000′ SS-ASy-D2-O

Travel protocols will be essential today. We will be choosing to travel one at a time and spacing out through avalanche terrain, paying close attention to utilizing safe zones well out of the way of the potential runout of avalanches, avoiding crowded slopes, and be digging test pits to improve the accuracy of our slope scale assessments and go-no-go decision making. Evaluate snow and terrain carefully avoiding the largest and broadest slopes and avoiding terrain traps.

Red flags:

  • Our primary red flag to look for today is upside-down snow. This indicates a flaw in the snowpack that should be completely avoided. Simple probe testing or pole testing can easily reveal stiffer snow overlying weaker snow. Areas with a right-side-up snowpack exist, and if found harvest it.
  • April has returned winter to us with amble new snow.  Our human desire to recreate in these conditions is a strong lure. Curbing your desire with a heightened approach will be key to your safety.
  • Recent avalanches shooting cracks and collapsing may not be present prior to triggering an avalanche.
  • It may take multiple riders to trigger an avalanche and this may mislead you in your safety assessment.

 

Avalanche Problem 2
  • Dry Loose
    Dry Loose
  • Aspect/Elevation
  • 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.

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

Dry loose avalanches (sluffs ) will be possible to human trigger on the northern half of the compass, west through east aspects (clockwise) at all elevations on steep convexities and rollovers in terrain 40º and steeper.  They are most hazardous if you are caught and carried into a terrain trap such as a gully, cliff, or couloir.  While most sluffs will be small, getting caught in steep terrain that funnels into any terrain trap has the potential to increase the size, risk and consequence of an avalanche.

Cooler overnight temperatures will keep snow surfaces dry and loose through most of the day on true north.  On aspects where dry unconsolidated snow sits on firm bed surfaces, sluffs will be more likely to trigger and result in a larger volume of debris. It will be possible to get caught and carried, injured, or tweek a knee in this terrain. Sluff management and mitigating a sluff may be challenging today due to the slow nature of the snow and inability to get enough speed to ski or ride fast enough to avoid or outrun debris.

WET AVALANCHES

With the combination of green-housing and/or sunshine in the forecast expect wet loose avalanches to be possible to human trigger in the afternoon on terrain 40º and steeper on the southern half of the compass, southeast through southwest aspects (clockwise). Slight shifts in aspect will determine whether a sluff is dry or wet and might start dry and end wet.  Timing your assents and descents will make all the difference for quality of skiing or riding today.

Weather
Sat, April 6th, 2024

 

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