Characteristics

The avalanche problem is related to current or most recent snowfall. The amount of additional loading by new snow onto the existing snowpack is the crucial factor of the new snow problem. How critical the loading is, depends on various factors such as air temperature, wind or characteristics of the old snow surface.

Avalanche type and trigger

• Dry-snow slab avalanches
• Dry loose snow avalanches
• Natural and human triggered avalanches possible

Spatial distribution

In general, a widespread presence and often on all aspects.

Position of the weak layer in the snowpack

Dry-snow slab avalanches:

Typically between new snow and old snow or within the new snow layers. Occasionally slightly below the old snow surface. In that case, the problem “persistent weak layers” additionally prevails.

Dry loose snow avalanches:

Start at the surface but the avalanche flow can erode deeper into the snowpack.

Release characteristics

Dry-snow slab avalanches:

Failure of newly-formed weak layers within the new snow or due to additional loading by snowfall on existing weak layers (old snow surface or below).

Dry loose snow avalanches:

Lack of cohesion between the new snow particles

Duration

Typically during snowfall and up to a few days after.

Identification of the problem in the field

The new snow problem is fairly easy to recognize since it affects most of the terrain but the characterization of the associated danger can be very tricky. Consider critical amounts of new snow and recent avalanche activity.

Travel advice

Dry-snow slab avalanches:

Wait until the snowpack has stabilized and the weak layer has gained strength.

Dry loose snow avalanches:

Danger of being carried away by small avalanches is more important than danger of burial. Consider consequences in extreme terrain.

Characteristics

Wind slabs are formed when loose snow in near-surface layers (new snow or old snow) is transported and deposited by wind.

Avalanche type and trigger

• Dry-snow slab avalanches
• Natural and human triggered avalanches possible

Spatial distribution

Highly variable but typically on leeward slopes, gullies and bowls, near distinct changes in slope angle, behind ridgelines or other wind-sheltered locations. More common above treeline.

Position of the weak layer in the snowpack

Typically between wind slab and old snow or within the wind slab layers due to variations in wind speed. Occasionally slightly lower in the old snowpack. In that case, the problem “persistent weak layers” additionally prevails.

Release characteristics

The wind slab is an additional load on a weak layer and builds a slab structure that is particularly prone to being triggered.

Duration

The wind slab problem can evolve very quickly. The problem lasts typically during the snowdrift event and tends to stabilize within a few days following the storm cycle.

Identification of the problem in the field

If not buried by new snow, the wind slab problem can be recognized with training and good visibility. Consider wind signs and locate snow drifted deposits. Typical clues: snow drifted deposits, recent avalanche activity and sometimes shooting cracks or whumpfs. However, it is often hard to determine the age of snow drifted deposits and wind signs do not necessarily imply an avalanche problem (e.g. in absence of a weak layer).

Travel advice

Avoid snow drifted deposits in steep terrain.

Characteristics

The avalanche problem is related to the presence of one or more persistent weak layers in the old snowpack. These weak layers typically include faceted crystals, depth hoar or surface hoar crystals.

Avalanche type and trigger

• Dry-snow slab avalanches
• Mostly human triggered avalanches; natural avalanches are rare, mainly in combination with other avalanche problems.
• Remote triggering is possible and crack propagation over long distances is common.

Spatial distribution

The avalanche problem can be widespread or quite isolated. It can exist in all aspects, but is more frequently found on shady, wind sheltered slopes.

Position of the weak layer in the snowpack

In the old snowpack, often deeply buried. However, when deeply buried triggering is less likely, but avalanches may become large.

Release characteristics

Avalanche release occurs when loading exceeds the strength of the weak layer.

Duration

Weak layers can persist for weeks to months; possibly even during most of the winter season.

Identification of the problem in the field

Persistent weak layers are very challenging to recognize. Signs of instability such as whumpfs are typical, but not necessarily present. Stability tests can be helpful to detect persistent weak layers. Knowledge of snowpack evolution is required and reference to the avalanche report is important.

Travel advice

Travel conservatively and avoid terrain features (e.g. large steep slopes) where consequences of being caught are large (e.g. deep burial). Consider the history of weather and snow cover processes in the area. Be extra cautious in areas with a thin snowpack and at the transition from thin to deep snowpack. The release of avalanches in persistent weak layers are a significant cause of recreational avalanche fatalities.

Characteristics

The avalanche problem is related to a weakening of the snowpack due to the presence of liquid water. Water infiltrates the snowpack due to melt or rain.

Avalanche type and trigger

• Wet-snow slab avalanches
• Wet loose snow avalanches
• Mainly natural avalanches

Spatial distribution

When water infiltration is due to melting, the problem is often specific to certain slope aspects (solar radiation) and elevations (air temperature).

In case of rain on snow, all slope aspects are affected (below the elevation, where snow turns to rain).

Position of the weak layer in the snowpack

Anywhere in the snowpack, in case of slab avalanches often at pre-existing weak layers.

Release characteristics

Wet-snow slab avalanches:

• Weakening and failure of pre-existing weak layers in the snowpack or release at layer interfaces due to ponding water.
• Rain represents also an additional load on weak layers.

Wet loose snow avalanches:

• Loss of cohesion between wet snow crystals

Duration

• Hours to days
• Rapid loss of stability possible
• Especially critical as water infiltrates for the first time deeper down, once the snowpack has warmed up to 0 °C.
• Natural avalanches might be more likely in the course of the day, depending on aspect (unless rain is the dominating factor).

Identification of the problem in the field

The wet snow problem is usually easy to recognize. Onset of rain, snowballing, pin wheeling and small wet slab or loose snow avalanches are often precursors of natural wet-snow avalanche activity. Deep foot- or ski-penetration is another sign of increased wetting.

Travel advice

If the wet snow surface freezes overnight due to clear skies and cold temperatures then develops a strong supporting crust, favourable conditions will usually be present in the morning. After warm, overcast nights, the problem will often be in existence in the morning. Normally rain on new snow creates this problem almost immediately. Good timing and trip planning are important. Consider avalanche runout zones.

Characteristics

The entire snowpack is gliding on the ground, typically on smooth ground such as grassy slopes or smooth rock zones. High activity of glide-snow avalanches is typically related to a thick snowpack with no or only few weak layers. Glide-snow avalanches can occur both with a cold dry snowpack and with a warm moist or wet snowpack. The release of a glide-snow avalanche is difficult to predict, although in many cases glide cracks open prior to release.

Avalanche types and trigger

• Glide-snow avalanches; cold dry or 0 °C‑isothermal wet snowpack
• Almost exclusively natural avalanches. Human and artificial triggering is very unlikely.

Spatial distribution

Primarily on smooth ground and on slopes of any aspect, but more often on sun-exposed slopes.

Position of the weak layer in the snowpack

Interface between the ground and overlaying snowpack

Release characteristics

Glide-snow avalanches are caused by a loss of friction at the snow-ground interface due to the presence of liquid water.

Duration

Days to months; occasionally during entire winter-season. The release can occur at any time during the day. In spring, glide-snow avalanches occur often during the second part of the day.

Identification of the problem in the field

The glide snow problem can often be recognized by the presence of glide cracks, which are often pre-cursors of glide snow avalanche release. However, the presence of glide cracks does not indicate imminent avalanche release, which is nearly impossible to predict. Avalanche release without pre-existing glide cracks is also common.

Travel advice

Avoid areas close to glide cracks.

Characteristics

A wave-like formation of soft or hard wind drifted snow, often overhanging.

Avalanche type and trigger

Cornice collapse can trigger new snow avalanches, wind slabs, persistent slabs, or wet avalanches on steep slopes below.

Spatial distribution

Cornices occur on the leeward sides of wind-exposed ridgelines or sharp terrain breaks.

Position of the weak layer in the snowpack

Snow drift extends the cornice outward, so the fresher, sensitive, and more easily triggered part of the cornice is generally near its outer edge.

Release characteristics

• Natural cornice collapses are common during windy midwinter storms, as cornices rapidly build outward and become unstable with drifting storm snow.
• Rapid warming, rainfall or prolonged melt can cause cornices to become unstable, to buckle and calve.

Duration

Once built, cornices can be an issue throughout the season, generally from midwinter through spring.

Identification of the problem in the field

Cornices occur on ridgelines or sharp terrain breaks and are usually easy to recognize. However, while standing on the top of cornices it is sometimes difficult to estimate their size. Cornices often break further back than expected, even onto flat terrain, and are the cause of many unexpected falls in the mountains.

Travel advice

Avoid travel on and below large ridge top cornices, especially during periods with drifting snow or the onset warm temperatures.

This is not a specific avalanche problem. It is a very inconclusive scenario, without a clear pattern that a user could follow to lower consequences. Any avalanche type is possible. Do not consider the absence of a typical avalanche problem as safe conditions. Normal caution is still advised.