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Avalanche bulletin through Wednesday, 1. February 2023
Wind slabs and weakly bonded old snow require caution
Edition: Tue 31.01., 17:00 Next update: Wed 01.02., 17:00 Validity
Avalanche bulletin through Wednesday, 1. February 2023
Wind slabs and weakly bonded old snow require caution
Edition Tue 31.01., 17:00 Next update Wed 01.02., 17:00 Validity
Avalanche bulletin through Wednesday, 1. February 2023
Wind slabs and weakly bonded old snow require caution
Edition Tue 31.01., 17:00 Next update Wed 01.02., 17:00 Validity
Avalanche bulletin through Wednesday, 1. February 2023
Wind slabs and weakly bonded old snow require caution
Edition Tue 31.01., 17:00 Next update Wed 01.02., 17:00 Validity
Moderate, Level 2+
Old snow, Snow drift
Avalanche prone locations
Danger level "moderate" (2+) in all aspects above 2200m. Other slopes about one danger level less.
Danger description
To some extent avalanches can be released in the old snowpack and reach medium size. These avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack.
In addition wind slabs formed in particular in gullies and bowls, and behind abrupt changes in the terrain. These are lying on the unfavourable surface of an old snowpack. Fresh and older wind slabs are to be evaluated with care and prudence.
Backcountry touring and other off-piste activities call for careful route selection.
Moderate, Level 2+
Snow drift, Old snow
Avalanche prone locations
Danger level "moderate" (2+) in all aspects above 2000m. Other slopes about one danger level less.
Danger description
As a consequence of a strong northwesterly wind, wind slabs formed in particular in gullies and bowls and behind abrupt changes in the terrain. They are rather small but in some cases prone to triggering. The fresh and older wind slabs are to be evaluated with care and prudence in steep terrain.
Avalanches can additionally in isolated cases be released in deeper layers also. These can in some cases reach medium size. Such avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack.
Apart from the danger of being buried, restraint should be exercised in particular in view of the danger of avalanches sweeping people along and giving rise to falls.
Moderate, Level 2=
Snow drift, Old snow
Avalanche prone locations
Danger level "moderate" (2=) in all aspects above 2200m. Other slopes about one danger level less.
Danger description
As a consequence of a strong northwesterly wind, wind slabs formed in particular in gullies and bowls and behind abrupt changes in the terrain. They are mostly small but in some cases prone to triggering. Fresh and older wind slabs are to be evaluated with care and prudence in particular in very steep terrain.
Avalanches can additionally in isolated cases be released in deeper layers also. These can in some cases reach medium size. Such avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack.
Backcountry touring and other off-piste activities call for careful route selection.
Moderate, Level 2-
Snow drift
Avalanche prone locations
Danger level "moderate" (2-) in all aspects above 2400m. Other slopes about one danger level less.
Danger description
As a consequence of a sometimes strong northwesterly wind, mostly small wind slabs formed. These are to be evaluated with care and prudence in particular in very steep terrain.
Careful route selection is recommended.
Low, Level 1
Snow drift
As a consequence of a sometimes strong northwesterly wind, mostly shallow wind slabs formed. The avalanche prone locations are to be found in particular in extremely steep terrain. Even a small avalanche can sweep people along and give rise to falls.
Snowpack
A little fresh snow in the central and eastern parts of the northern flank of the Alps and a strong to storm force northwesterly wind have given rise to snow drift accumulations over a wide area. The drifting snow has been deposited on the old snow surface, which is faceted in many places, or on surface hoar, and is therefore prone to triggering. In many cases the accumulations are hard and recognisable to the trained eye. Where the wind has exerted an influence adjacent to ridgelines and in pass areas, the fresh snow drift accumulations are less prone to triggering.
From southern Valais through the Gotthard region to Grisons, numerous soft faceted layers exist in the snowpack between compacted layers and crusts. These faceted layers are especially prevalent in places with shallow snow cover, where the snowpack can be penetrated down to the ground by skis. On the northern flank of the Alps the base of the snowpack is well bonded in many instances, but multiple faceted layers exist nearer the surface. The bonding of the snowpack is most favourable in the extreme west of Lower Valais and in northern Lower Valais.
From southern Valais through the Gotthard region to Grisons, numerous soft faceted layers exist in the snowpack between compacted layers and crusts. These faceted layers are especially prevalent in places with shallow snow cover, where the snowpack can be penetrated down to the ground by skis. On the northern flank of the Alps the base of the snowpack is well bonded in many instances, but multiple faceted layers exist nearer the surface. The bonding of the snowpack is most favourable in the extreme west of Lower Valais and in northern Lower Valais.
Observed weather review Tuesday, 31.01.2023
On Monday night a little snow fell in the northeast. The north and east were sunny for a time once the residual cloud dispersed, before becoming increasingly cloudy again in the afternoon. The south was mostly sunny.
Fresh snow
In the period from Monday evening until Tuesday morning, approximately 5 to 10 cm of snow fell, locally as much as 15 cm, in the central and eastern parts of the northern flank of the Alps and in northern Grisons and northern Lower Engadine.
Temperature
At midday at 2000 m: about -4 °C in the north and +1 °C in the south
Wind
During the night
- Moderate, sometimes strong, from westerly directions
- At elevated altitudes and in the south, strong to storm force from northerly directions
- Light to moderate from westerly directions
- At elevated altitudes, moderate, on the main Alpine ridge and in the east, sometimes strong, from the northwest
Weather forecast through Wednesday, 01.02.2023
On Wednesday the weather will be changeable. In the northeast a few centimetres of snow will fall above 600 m during the night and in the daytime. As the day progresses, cloud will build up from the north; sunny weather will persist longer in the inneralpine regions and the south.
Fresh snow
-
Temperature
At midday at 2000 m: about -7 °C in the north and -2 °C in the south
Wind
- Moderate to strong from westerly directions
- At elevated altitudes and in the south, strong from the northwest
Outlook through Friday, 03.02.2023
Thursday
On Wednesday night, snowfall will arrive from the northwest. During the day, snow will fall over a wide area and in some cases persistently. The snowfall level will be approximately 700 m. By the evening, 20 to 30 cm of snow will fall in the central and eastern parts of the northern flank of the Alps and in northern Grisons. Elsewhere 5 to 15 cm of snow will fall over a wide area, but it will remain dry in the far south. A strong, sometimes storm force northwesterly wind will persist.
As a consequence of fresh snow, wind and the unfavourable old snow surfaces, the avalanche danger will increase significantly in the north as the day progresses. In the south it will not change significantly.
As a consequence of fresh snow, wind and the unfavourable old snow surfaces, the avalanche danger will increase significantly in the north as the day progresses. In the south it will not change significantly.
Friday
It will be very cloudy and, in the period to Friday morning, snow will continue to fall over a wide area in the north. The snowfall level will rise from 700 m towards 1000 m. As the day progresses, the snowfall will ease from the west. By the evening a further 10 to 20 cm of snow will fall in the central and eastern parts of the northern flank of the Alps and in northern Grisons. The wind will ease a little, but at elevated altitudes and in the south will remain strong from the northwest.
As a consequence of fresh snow and wind, the avalanche danger will continue to increase in central and eastern parts of the northern flank of the Alps and in parts of Grisons. In the other regions it will not change significantly.
As a consequence of fresh snow and wind, the avalanche danger will continue to increase in central and eastern parts of the northern flank of the Alps and in parts of Grisons. In the other regions it will not change significantly.
Your observations can improve the quality of the avalanche bulletin. We are very grateful for any reports and photos received.
Please report your observations of avalanches or alarm signs, or your estimation of the avalanche danger, or simply send us a picture illustrating the current situation. Your report from the field will be considered along with all the other information when we assess the avalanche danger. It is impossible, however, to reflect the exact content of each individual report in the avalanche bulletin.
The best way to file a report is by completing the interactive form on this page. If your report is to be used in the 5 pm avalanche bulletin, it should be submitted before 2:30 pm if possible. Reports received later will normally be given consideration in the next assessment.
Other reporting options:
- White Risk App
- E-mail to bulletin(at)slf.ch
- Freephone number 0800 800 187
Snowpack
A little fresh snow in the central and eastern parts of the northern flank of the Alps and a strong to storm force northwesterly wind have given rise to snow drift accumulations over a wide area. The drifting snow has been deposited on the old snow surface, which is faceted in many places, or on surface hoar, and is therefore prone to triggering. In many cases the accumulations are hard and recognisable to the trained eye. Where the wind has exerted an influence adjacent to ridgelines and in pass areas, the fresh snow drift accumulations are less prone to triggering.
From southern Valais through the Gotthard region to Grisons, numerous soft faceted layers exist in the snowpack between compacted layers and crusts. These faceted layers are especially prevalent in places with shallow snow cover, where the snowpack can be penetrated down to the ground by skis. On the northern flank of the Alps the base of the snowpack is well bonded in many instances, but multiple faceted layers exist nearer the surface. The bonding of the snowpack is most favourable in the extreme west of Lower Valais and in northern Lower Valais.
From southern Valais through the Gotthard region to Grisons, numerous soft faceted layers exist in the snowpack between compacted layers and crusts. These faceted layers are especially prevalent in places with shallow snow cover, where the snowpack can be penetrated down to the ground by skis. On the northern flank of the Alps the base of the snowpack is well bonded in many instances, but multiple faceted layers exist nearer the surface. The bonding of the snowpack is most favourable in the extreme west of Lower Valais and in northern Lower Valais.
Observed weather review Tuesday, 31.01.2023
On Monday night a little snow fell in the northeast. The north and east were sunny for a time once the residual cloud dispersed, before becoming increasingly cloudy again in the afternoon. The south was mostly sunny.
Fresh snow
In the period from Monday evening until Tuesday morning, approximately 5 to 10 cm of snow fell, locally as much as 15 cm, in the central and eastern parts of the northern flank of the Alps and in northern Grisons and northern Lower Engadine.
Temperature
At midday at 2000 m: about -4 °C in the north and +1 °C in the south
Wind
During the night
- Moderate, sometimes strong, from westerly directions
- At elevated altitudes and in the south, strong to storm force from northerly directions
- Light to moderate from westerly directions
- At elevated altitudes, moderate, on the main Alpine ridge and in the east, sometimes strong, from the northwest
Weather forecast through Wednesday, 01.02.2023
On Wednesday the weather will be changeable. In the northeast a few centimetres of snow will fall above 600 m during the night and in the daytime. As the day progresses, cloud will build up from the north; sunny weather will persist longer in the inneralpine regions and the south.
Fresh snow
-
Temperature
At midday at 2000 m: about -7 °C in the north and -2 °C in the south
Wind
- Moderate to strong from westerly directions
- At elevated altitudes and in the south, strong from the northwest
Outlook through Friday, 03.02.2023
Thursday
On Wednesday night, snowfall will arrive from the northwest. During the day, snow will fall over a wide area and in some cases persistently. The snowfall level will be approximately 700 m. By the evening, 20 to 30 cm of snow will fall in the central and eastern parts of the northern flank of the Alps and in northern Grisons. Elsewhere 5 to 15 cm of snow will fall over a wide area, but it will remain dry in the far south. A strong, sometimes storm force northwesterly wind will persist.
As a consequence of fresh snow, wind and the unfavourable old snow surfaces, the avalanche danger will increase significantly in the north as the day progresses. In the south it will not change significantly.
As a consequence of fresh snow, wind and the unfavourable old snow surfaces, the avalanche danger will increase significantly in the north as the day progresses. In the south it will not change significantly.
Friday
It will be very cloudy and, in the period to Friday morning, snow will continue to fall over a wide area in the north. The snowfall level will rise from 700 m towards 1000 m. As the day progresses, the snowfall will ease from the west. By the evening a further 10 to 20 cm of snow will fall in the central and eastern parts of the northern flank of the Alps and in northern Grisons. The wind will ease a little, but at elevated altitudes and in the south will remain strong from the northwest.
As a consequence of fresh snow and wind, the avalanche danger will continue to increase in central and eastern parts of the northern flank of the Alps and in parts of Grisons. In the other regions it will not change significantly.
As a consequence of fresh snow and wind, the avalanche danger will continue to increase in central and eastern parts of the northern flank of the Alps and in parts of Grisons. In the other regions it will not change significantly.
Have you observed alarm signs or an avalanche?
Your observations can improve the quality of the avalanche bulletin. We are very grateful for any reports and photos received.
More information about observations
Please report your observations of avalanches or alarm signs, or your estimation of the avalanche danger, or simply send us a picture illustrating the current situation. Your report from the field will be considered along with all the other information when we assess the avalanche danger. It is impossible, however, to reflect the exact content of each individual report in the avalanche bulletin.
The best way to file a report is by completing the interactive form on this page. If your report is to be used in the 5 pm avalanche bulletin, it should be submitted before 2:30 pm if possible. Reports received later will normally be given consideration in the next assessment.
Other reporting options:
- White Risk App
- E-mail to bulletin(at)slf.ch
- Freephone number 0800 800 187
No avalanche bulletin is published currently. Nevertheless, you should still stay up to date with the avalanche situation in the mountains, especially if there is fresh snow.
However, the SLF will, by way of exception, also issue avalanche bulletins in the summer in case of heavy snowfall. There are different ways you can be notified when these bulletins based on the snow situation are published:
- by push alert on SLF's free White Risk mobile app: appearing in four languages (English, German, French and Italian), this can be downloaded from iTunes App Store (for iPhones) or Google Play Store (for Android);
- via an RSS feed which informs you whenever an avalanche bulletin is published.
Depending on the snow and avalanche situation, the regular publication of avalanche bulletins recommences in November/December.
Have you observed alarm signs or an avalanche?
Your observations can improve the quality of the avalanche bulletin. We are very grateful for any reports and photos received.
More information about observations
Please report your observations of avalanches or alarm signs, or your estimation of the avalanche danger, or simply send us a picture illustrating the current situation. Your report from the field will be considered along with all the other information when we assess the avalanche danger. It is impossible, however, to reflect the exact content of each individual report in the avalanche bulletin.
The best way to file a report is by completing the interactive form on this page. If your report is to be used in the 5 pm avalanche bulletin, it should be submitted before 2:30 pm if possible. Reports received later will normally be given consideration in the next assessment.
Other reporting options:
- White Risk App
- E-mail to bulletin(at)slf.ch
- Freephone number 0800 800 187
Danger levels
The SLF uses the five-level European avalanche danger scale to denote the avalanche danger. However, in reality the avalanche danger changes gradually. This means there is a range within each level. The subdivisions allow the unfolding danger situation to be tracked more accurately. The avalanche warning service communicates with it where within the range it assesses the current danger.
Avalanche danger scale
Short version
Danger level | Characteristics | Recommendations for backcountry recreationists |
5 very high | Extraordinary avalanche situation Numerous very large and extremely large natural avalanches can be expected. These can reach roads and settlements in the valley. | You are advised not to engage in winter sports beyond open ski runs and trails. Very rarely forecast. Around 1 % of avalanche fatalities. |
4 high | Very critical avalanche situation Natural and often very large avalanches are likely. Avalanches can easily be triggered on many steep slopes. Remote triggering is typical. Whumpf sounds and shooting cracks occur frequently. | Stay on moderately steep terrain. Heed runout zones of large avalanches. Unexperienced persons should remain on open ski runs and trails. Forecast only on a few days throughout the winter. Around 10 % of avalanche fatalities. |
3 considerable | Critical avalanche situation Whumpf sounds and shooting cracks are typical. Avalanches can easily be triggered, particularly on steep slopes with the aspect and elevation indicated in the avalanche bulletin. Natural avalanches and remote triggering can occur. | The most critical situation for backcountry recreationists. Select best possible route and take action to reduce risks. Avoid very steep slopes with the aspect and elevation indicated in the avalanche bulletin. Unexperienced persons are advised to remain on open ski runs and trails. Forecast for around 30 % of the winter season. Around 50 % of avalanche fatalities. |
2 moderate | Mostly favourable avalanche situation Warning signs can occur in isolated cases. Avalanches can be triggered in particular on very steep slopes with the aspect and elevation indicated in the avalanche bulletin. Relatively large natural avalanches are not to be expected. | Routes should be selected carefully, especially on slopes with the aspect and elevation indicated in the avalanche bulletin. Travel very steep slopes one person at a time. Pay attention to unfavourable snowpack structure (persistent weak layers, old snow problem). Forecast for around 50 % of the winter season. Around 30 % of avalanche fatalities. |
1 low | Generally favourable avalanche situation No warning signs present. Avalanches can only be triggered in isolated cases, in particular on extremely steep slopes. | Travel extremely steep slopes one person at a time and be alert to the danger of falling. Forecast for around 20 % of the winter season. Around 5 % of avalanche fatalities. |
Full description of the European avalanche danger scale
This scale, introduced by the European Avalanche Warning Services on winter 1993/94, defines the danger level based on the snowpack stability and the avalanche triggering probability. The full description of the scale also includes other columns that have not been internationally agreed relating to typical characteristics, recommendations and consequences.
European Danger Scale with recommendations and additions (.pdf)
Subdivisions
When there is a moderate or higher danger of dry-snow avalanches (starting from level 2), the SLF subdivides the points on the European avalanche danger scale. These subdivisions indicate whether the danger is estimated to be towards the bottom end (-), more or less in the middle (=) or towards the top end (+) of the forecast level.
Danger levels – a simplified picture of reality
The avalanche danger does not increase in linear fashion from one level to another, but disproportionately. As the danger level increases,
- snowpack stability, and therefore the additional load required to trigger an avalanche, decreases. In consequence, the probability of an avalanche triggering increases.
- the prevalence of avalanche prone locations increases. In other words, there are more places where avalanches can release naturally or be triggered.
- avalanche size increases as well, in particular when the danger level is at the higher end of the scale.
If the additional load required to trigger an avalanche decreases and there are also more locations where avalanches can be triggered, the avalanche triggering probability increases. This is also shown by the stability distribution in the chart below.
In a typical case, all these influencing variables change as indicated above. This means that in the case of 'low' avalanche danger, usually only small avalanches are triggered in just a few locations and mostly only due to a high additional load, while in the case of 'high' avalanche danger, a lot of avalanches, some of them very large, are triggered or are released naturally (without human influence).
However, there are also atypical situations that do not fit into this picture. These are detailed in the next section.
Various characteristics of avalanche danger
Also in the case of less typical avalanche situations the danger level is a measure of the order of magnitude of the avalanche danger. These situations are detailed below along with information about their assessment by the avalanche warning service. As these are atypical situations, no list can ever be exhaustive. In atypical situations deviations from the danger level definition are inevitable. These are set out as far as possible in the avalanche bulletin's danger description.
Faceted-crystal snowpack
In the case of low avalanche danger (level 1) the snowpack is normally well bonded and stable. However, after long periods of fine weather with shallow snow, another form of snow occurring in mid-winter which makes slab avalanches virtually impossible is the whole snowpack being loose and transformed into faceted crystals. The snowpack is then very weak and there are also weak layers, but the bonded layer on top (the 'slab') is lacking. With no bonded layer a fracture cannot be propagated, meaning that there is no possibility of a slab avalanche forming. This means there is a low avalanche danger (level 1), despite or precisely because of the very loose snowpack. 'Stable snowpack' means 'not liable to trigger slab avalanches' and does not refer to the hardness of the layers.
This situation is not a good omen for the immediate future, given that as soon as it is snowed on, the fresh-fallen snow and fresh snowdrift result in the creation of a 'slab' where one did not exist before. Underneath this is the loose old snowpack in the form of a substantial weak layer. The avalanche danger will increase significantly, generally resulting in a long-lasting old-snow problem.
Small, easily triggered snowdrift accumulations
Fresh snowdrift accumulations can often be triggered by individual winter sports enthusiasts. The size of the snowdrift accumulations depends not only on the wind but also on the supply of fresh and old snow which can be transported. For only little snow which can be transported, the snowdrift accumulations are usually so small that getting buried by them is unlikely. In this case, level 2 (moderate) is often used despite the high probability of an avalanche release. In such situations the snowdrift accumulations can usually be seen in good visibility by the trained eye. They need to be avoided especially on terrain where there is a danger of falling.
Old-snow problem with a significant weak layer deep down in the snowpack
The more thickly a weak layer is covered, the more difficult it becomes for a fracture to form there. This is most likely to occur in locations where the snow is relatively shallow or in transitions from shallow to deep snow. In the case of an old-snow problem with a significant weak layer deep down in the snowpack, avalanche prone locations are usually relatively rare. However, avalanches often reach large size, and are therefore particularly dangerous for winter sports enthusiasts. Therefore, the avalanche danger in the case of an old snow problem can sometimes be considerable (level 3) even if the avalanche prone locations are fairly rare. An aggravating factor is that the avalanche prone locations are barely recognisable in old snow situations, even to the trained eye. In the case of weak old snow, more fatalities can be expected than in the case of the other avalanche problems (at the same danger level).
'Skier high'
If numerous large and, in many cases, very large-sized natural avalanches can be expected, the avalanche danger is classified as ‘high’ (level 4). In these circumstances, exposed objects (mostly sections of transportation routes, but also buildings in isolated cases) can be endangered. Alongside this classic ‘road high’ situation there is a further variant of this danger level when, even though very large avalanches are unlikely to occur, there are a lot of places where people can very easily trigger medium and large-sized avalanches. In many such cases, avalanches are released naturally as well. When this ‘skier high’ situation exists, those engaging in winter sports beyond the boundaries of marked and secured pistes are in acute danger. Transportation routes, in contrast, are either unaffected or affected only in isolated cases. When ‘skier high’ applies, the danger is usually described with the subdivision 4- or 4=; in the case of ‘road high’, any of the subdivisions can be used.
Avalanche activity in case of wet and gliding snow
Wet-snow avalanches are seldom triggered by people, and in the case of gliding avalanches this is virtually impossible. Therefore, natural triggering is the main cause of such avalanche types even in the when lower danger levels prevail. The maximum possible naturally triggered avalanche activity, based on the defined danger level, relates mainly to wet-snow and gliding-snow conditions and less to conditions involving dry avalanches. In this context large natural avalanches are possible when there is a moderate danger of wet-snow or gliding avalanches. In the case of a situation with dry-snow avalanches, such naturally triggered avalanche activity normally corresponds to a considerable avalanche danger, as then avalanches are also expected to be triggered by individuals.
Change in the avalanche danger as the day progresses
The avalanche danger changes over time and may not reach or overshoot the boundary between one danger level and another within the period of validity of the avalanche bulletin. Ordinarily the danger increases, for example because snowfall or wind, significantly faster than it recedes again.
If the danger level is likely to change during the day, the level published in the avalanche bulletin and the danger description normally show the situation in the morning. The change (often an increase) is indicated in the danger description. Here are some examples:
- "The avalanche danger will increase and reach level 3 (considerable) in the afternoon." In this case, level 2 (moderate) is marked on the hazard map.
- "Danger level 4 (high) will be reached during the morning." In this case, level 4 (high) is marked on the hazard map.
- "As a consequence of daytime warming and solar radiation, wet-snow avalanches can be expected as the day progresses below approximately 2400 m." (With no danger level indicated)
If the avalanche danger is assessed to be level 4 (high) or even level 5 (very high) at night, and then one level lower during the day, the morning rule is deviated from. As when transport routes are endangered, the avalanche danger is also significant at night, the higher avalanche level that applies during the night is given in the evening edition. In the morning edition this is then reduced to the level applying in the morning.
Double map
In typical springtime conditions, the danger of wet-snow avalanches along with daytime warming and solar radiation will increase significantly as the day progresses. During the day the danger of dry-snow avalanches will usually only change slightly in these conditions. Thus, while in the morning dry-snow avalanches are the main danger, in the afternoon the main danger is posed by wet-snow avalanches. In this situation, two maps show both the more favourable morning situation (dry-snow avalanches) and the unfavourable situation in the afternoon (wet-snow avalanches as the day progresses). The transition from one map to another cannot be pinned down to a specific time. It depends on the conditions and the altitude and also in particular the aspect. Whereas on east-facing slopes the danger of wet-snow avalanches will already increase during the morning, this usually occurs only later on west-facing slopes.
In special cases a double map is also used if there is a significant danger of gliding avalanches, and this danger is greater, over a wide area, than the danger of dry slab avalanches. It is worth noting in this case that these two dangers do not vary significantly during the day. Therefore, the two avalanche types are possible throughout the day.
Additional information
Avalanche danger and risk
The avalanche bulletin describes the avalanche danger, i.e. the likelihood of a release and the possible size of avalanches in a specific region, but the exact timing of an avalanche being triggered and the actual length of its starting zone and fracture depth cannot be determined.
An avalanche danger only becomes a risk (i.e. a probability that damage will occur) if endangered individuals, animals, forest, infrastructure etc. are in the area of the potential avalanche. In the avalanche bulletin, the avalanche danger is assessed regardless of the presence of endangered individuals or objects, i.e. on weekends with fine weather and weekdays with poor weather alike, and for populated areas and outlying terrain alike.
If an avalanche is released somewhere on a glacier during a snowstorm, there would obviously be an avalanche danger, but there would be no risk if there were no people in the surrounding area. If the same avalanche is released on a popular touring route on a sunny weekend, the risk would be much greater. The danger given in the avalanche bulletin may be the same in both cases, but the risk will be different.
Avalanches are a very special natural hazard, since unlike flash floods or earthquakes the 'perilous process' of an avalanche can be initiated by human activity. If anyone comes onto a dangerous slope, the artificial additional load can trigger an avalanche. In the case of more than 90% of the snow sports enthusiasts buried by a slab avalanche, they triggered the avalanche themselves or it was triggered by another member of their group.
Frequency of danger levels
Danger level 2 (moderate) is forecast in the Alps on two out of five days in each warning region. It is the most frequently cited danger level and describes days on which the avalanche danger is about “average”. Level 3 (considerable) is forecast on around one in three days. Danger level 4 (high) applies on just 2.2% of winter days on average, and level 5 (very high) is forecast only extremely seldom. In the Jura, the lower danger levels apply more frequently.
Further Information
Division into regions
For the purposes of the avalanche bulletin, the Swiss Alps are divided in alignment with the warning regions used by the other federal natural hazard agencies (MeteoSwiss, Federal Office for the Environment (FOEN), Swiss Seismological Service (SED)). Groups consisting of several warning regions are formed, generally by applying climatological or political criteria, yielding overarching region names (see the maps below).
Great care is required when interpreting references in the context of backcountry tours in regional border areas. For example, the Jungfrau region is usually accessed from the north (northern flank of the Alps or Bernese Oberland), but the backcountry touring area mostly lies in Valais.
Marginal areas
There are no clearly defined boundaries between two regions with different danger assessments (e.g. different danger levels or different distributions of avalanche prone locations) but instead transitional areas which in many cases cannot be clearly assigned to either avalanche situation. This means that in a marginal area several kilometres wide, it can be assumed that either the more or the less favourite situation may apply.
Those undertaking backcountry ski or snowshoe hiking tours in such areas should therefore consult the avalanche bulletin for both regions in question.
Warning regions (the 149 smallest units)
Northern and southern flanks of the Alps, and the Jura
Main Alpine Ridge, Northern Alpine Ridge and Inneralpine Regions
The Main Alpine Ridge extends from Val Ferret via the Great St Bernard, Monte Rosa, Simplon, Gotthard, Lukmanier, San Bernardino, Maloja and Bernina passes to beyond Val Müstair.
The Northern Alpine Ridge covers a belt running from the Dent du Midi via the Wildstrubel and Jungfrau regions and Gotthard, Tödi and Vorab to Liechtenstein.
The Inneralpine Regions encompass the regions between the Main Alpine Ridge and the Northern Alpine Ridge, namely those of Central Valais, and parts of Northern and Central Grisons and Engadine.
Major political regions
The Grisons southern valleys consist of Val Mesolcina and Val Calanca (collectively Moesano), Val Bregaglia, Val Poschiavo and Val Müstair.
Political subregions 1
Political subregions 2
The Gotthard region consists of Obergoms, the Grimsel region, Urseren, Tavetsch, the Upper Valle Leventina and Val Bedretto.
Division into regions
For the purposes of the avalanche bulletin, the Swiss Alps are divided in alignment with the warning regions used by the other federal natural hazard agencies (MeteoSwiss, Federal Office for the Environment (FOEN), Swiss Seismological Service (SED)). Groups consisting of several warning regions are formed, generally by applying climatological or political criteria, yielding overarching region names (see the maps below).
Great care is required when interpreting references in the context of backcountry tours in regional border areas. For example, the Jungfrau region is usually accessed from the north (northern flank of the Alps or Bernese Oberland), but the backcountry touring area mostly lies in Valais.
Marginal areas
There are no clearly defined boundaries between two regions with different danger assessments (e.g. different danger levels or different distributions of avalanche prone locations) but instead transitional areas which in many cases cannot be clearly assigned to either avalanche situation. This means that in a marginal area several kilometres wide, it can be assumed that either the more or the less favourite situation may apply.
Those undertaking backcountry ski or snowshoe hiking tours in such areas should therefore consult the avalanche bulletin for both regions in question.
Warning regions (the 149 smallest units)
Northern and southern flanks of the Alps, and the Jura
Main Alpine Ridge, Northern Alpine Ridge and Inneralpine Regions
The Main Alpine Ridge extends from Val Ferret via the Great St Bernard, Monte Rosa, Simplon, Gotthard, Lukmanier, San Bernardino, Maloja and Bernina passes to beyond Val Müstair.
The Northern Alpine Ridge covers a belt running from the Dent du Midi via the Wildstrubel and Jungfrau regions and Gotthard, Tödi and Vorab to Liechtenstein.
The Inneralpine Regions encompass the regions between the Main Alpine Ridge and the Northern Alpine Ridge, namely those of Central Valais, and parts of Northern and Central Grisons and Engadine.
Major political regions
The Grisons southern valleys consist of Val Mesolcina and Val Calanca (collectively Moesano), Val Bregaglia, Val Poschiavo and Val Müstair.
Political subregions 1
Political subregions 2
The Gotthard region consists of Obergoms, the Grimsel region, Urseren, Tavetsch, the Upper Valle Leventina and Val Bedretto.
Social media
Further information on the avalanche bulletin and avalanche danger, interesting facts about WhiteRisk and much more at @whiteriskslf:
