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SLF: From 22/23 intermediate stages in the bulletin

The SLF introduces a finer subdivision for hazard levels 2, 3, 4 and 5

by Lea Hartl 11/28/2022
What experienced skiers could more or less reliably glean from the text of the bulletin is now put into concrete figures. From this season onwards, the SLF will use three intermediate levels for the avalanche danger levels moderate, considerable, large and very large. For level 3, for example, a 3, 3= or 3+ is given in addition to the "whole" level (3, considerable). 3- is closer to 2, 3= is "neutral" and 3+ is closer to 4.

Intermediate levels: Frequently requested by users

Anyone who spends a lot of time on tour or freeriding will know that a "considerable" can feel quite dark orange on some days, while on other days it feels more like a "moderate". From a practical skiing perspective, it therefore seems obvious to differentiate the five-level danger scale more precisely. In the text of the Swiss bulletin (and also in the situation reports of many neighboring countries), the severity and level of danger are often described more precisely than just with the level. For example, a textual distinction between "winter sports four" and "infrastructure four" has become increasingly common in recent years.

The desire for a more precise subdivision in the bulletin - not only in the text, but also in figures - has been repeatedly brought to the SLF, according to Kurt Winkler, SLF avalanche warning officer. For six winters now, SLF forecasters have been estimating intermediate stages in addition to the usual contents of the bulletin, but these have not been publicly available until now. After several years of internal testing, extensive statistical evaluations and two scientific publications, the intermediate levels are now ready for regular use in the bulletin.

From theory to practice

A subdivision of the hazard levels doesn't sound particularly complicated at first, but the path to the operational version was long and laborious. One thing was clear: the SLF wanted to respond to users' requests for a more precise subdivision. But how do you go about it?

First, a theoretical basis had to be found on which the practical implementation could be built. When people categorize something, they can only do so in about five to a maximum of seven defined classes. More is too much, we are then no longer able to differentiate meaningfully between the classes. It is therefore not expedient to extend the five-level danger scale by several whole levels. Apart from these psychological factors, a change to the five-level scale would also be neither politically realistic nor desirable, according to Winkler (compatibility with standards of other Swiss natural hazards and the EAWS - European Association of Avalanche Warning Services).

In contrast, a subdivision within individual hazard levels seemed to be consistent in terms of decision-making theory and could also be implemented at all other levels. After all, people are quite capable of determining a relative ranking within a class after it has been divided into defined classes. Winkler, who played a key role in the introduction of the intermediate levels, explains the concept using the example of fast food restaurants: "Fast food is the defined restaurant class and is objectively differentiated from other classes such as Michelin-starred restaurants. Within the fast food class, I decide on a restaurant based on a subjective ranking, for example because I prefer to go to McDonalds rather than Burgerking or vice versa. The subjective ranking exists within the objective class and does not change it.

The principle of "fast and slow thinking" made famous by Daniel Kahneman also comes into play in the intermediate stages. Here, fast, heuristic, instinctive thinking contrasts with slower, more logical, rule-based considerations. The five known avalanche danger levels result from the latter: The definitions of the scale and the EAWS matrix specify the class and the creation of the levels follows known, objective rules. Within the defined classes of danger levels, a subjective ranking can now be created in the form of intermediate levels. The progonostics determine them more or less by feel, without following a concrete set of rules. First, the entire level is determined (e.g. 3, considerable). If this is unambiguous, the middle, neutral sub-level is added to the whole level (3=). However, if the forecasters find that "today is a sharp three", or "the four is not quite so tricky this time, this is almost a three", then level 3 is given the addition 3+, or level 4 is supplemented by a 4-.

This additional information (e.g.: critical three) was already contained in the text before, so it is not fundamentally new content. It is also not surprising that avalanche warnings are able to assess the danger in a more differentiated way than the five-point scale allows. Winkler emphasizes that the knowledge with which the intermediate levels are intuitively created must be available anyway in order to write the textual summary of the avalanche situation in the bulletin. However, the intermediate levels now present the underlying information in a more categorical and consistent way.

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Do the sub-levels really work?

So that's the theory: a subjective "top, middle, bottom" ranking is created within the defined, complete hazard levels. But does this really work? And if so, how well? And what does "work" actually mean?

The standardized avalanche danger level scale in Europe is a success story of international niche diplomacy. The path to a common system was laborious and deviations from it need to be carefully considered, even if it is not a matter of fundamentally different categories, but "only" a refinement with intermediate levels. Accordingly, the intermediate stages in the current bulletin were preceded by a long verification process. According to Kurt Winkler, the introduction of the intermediate stages is probably the first major innovation in the bulletin where it was tested beforehand whether and how well the new method works.

The quality analysis of forecasts of any kind generally boils down to a comparison of the forecast with reality in the forecast period. This is not so easy in the case of avalanche danger, as it is not possible to use measuring instruments to verify whether the forecast is correct, as is the case with weather reports, for example. However, the SLF's extensive observer system offers a way to compare the forecast with local "nowcasts" from the observers (PG conditions reporter Alex was on tour with an SLF observer last season). The nowcasts are estimates of the avalanche danger at the time of observation, meaning that more up-to-date information is taken into account than at the time of the forecast.

In a first study, Winkler's team colleague Frank Techel shows that the differences between the nowcasts of the observers and the forecasts become smaller if the forecast contains intermediate stages. The nowcasts use the known 5 hazard levels and can be compared with the levels and intermediate levels of the bulletin. If the hazard level in the nowcast matches that of the forecast, it is not possible to assess whether the intermediate levels in the forecast provide any additional information. Sometimes, however, the nowcast deviates from the forecast and issues level 2, for example, while the forecast predicted level 3. If the intermediate stage in the forecast was 3 in this case, i.e. a less critical "significant", the deviation between the forecast and nowcast is reduced. The evaluation of the internally issued intermediate stages of recent winters clearly shows that the forecast and nowcast are closer together when intermediate stages are used.

A further study examines the relationship between the intermediate stages and more objective parameters such as snowpack stability and avalanches. In this case, too, it is not so easy to make the connection between these parameters and the danger level or the intermediate levels tangible in figures. The challenge starts again with the data situation: In order to quantify the snowpack stability and its distribution, observational data (powderguide noises, stability tethers such as slide block or ECT), modeling as well as the risk calculated from accident data and GPS tracks (see also: Study on the dependence of risk on hazard level and terrain) are used. First, it was determined how all these parameters correlate with the overall hazard levels. As expected, the "hazard parameters" increase with increasing hazard level, but some parameters are only suitable for assessing a certain range of the scale. As hoped, the intermediate levels also increase with the hazard parameters. The conclusion is therefore once again: with the information available in Switzerland, forecasters are able to differentiate more accurately within the 5-level scale.

Benefits and application in practice

After the theoretical foundations and comprehensive statistical evaluations, which confirm that the theory works, the intermediate levels are now available in the regular bulletin. This fulfills the users' wish for a more precise subdivision without creating any incompatibility with the five-level system. Intermediate levels are neither permitted nor prohibited in the EAWS, says Kurt Winkler. He sees the innovation as an optional addition to the existing hazard levels and assumes that some other warning services will also introduce intermediate levels in the coming years. As the intermediate levels do not change the existing system per se, but are an optional addition and, given the right conditions (data basis, resources of the warning services, ...), they are not in conflict with efforts to create a more uniform avalanche warning system throughout the Alps. In this context, Kurt Winkler understands "uniform" to mean that "the same is done the same", but not that everything must remain at the current level and no more innovations are possible.

The intermediate levels clearly indicate what winter sports enthusiasts have been able to infer more or less well from the text of the hazard description. The intermediate levels can be easily applied using standard decision support tools such as the reduction method or the Snowcard. With the graphical reduction method and the snowcard, the color scale allows you to shift in the direction of - or +, while the professional reduction method adjusts the hazard potential accordingly. The Austrian Alpine Association's Stop or Go method cannot be used in the same way, but here too the intermediate levels naturally provide useful information that can be taken into account in addition to the Stop or Go checks, for example.

The intermediate levels are already used in computer models. They were already integrated into Skitourenguru in winter 2019, where they are included in the automatic risk calculation. Kurt Winkler also emphasizes the great potential for the use of intermediate stages in numerical models used to calculate avalanche risk. There is ongoing research on this at the SLF and the first exciting publications (Avalanches and artificial intelligence). Algorithms based on machine learning need comprehensive and high-quality training data sets in order to learn what they are supposed to learn. The refined risk assessment using intermediate stages increases the information content of the training data available to the models. This in turn improves the model result.

Conclusion

Like all other content in modern bulletins and avalanche situation reports, the intermediate stages were developed to increase the usefulness of the forecast for users. Users are people, but also algorithms such as Skitourenguru and "artificial intelligence" (models), which help avalanche warnings assess the avalanche danger.

The example of substages shows how complex supposedly simple changes and innovations in avalanche warning can be. Few other warning services are as well positioned as the SLF in terms of information density from the terrain and other resources. It will therefore be interesting to see in which regions the new system will be adopted in the future. In any case, the technical foundations have been laid.

We are looking forward to the first winter with intermediate stages in the Swiss bulletin and look forward to feedback from the PG community! Let us know if and how you consider the intermediate stages in your tour planning and how you are doing in the terrain!

Further reading:

Report on the intermediate stages at the SLF

Refined dry-snow avalanche danger ratings in regional avalanche forecasts: Consistent? And better than random? Techel et al., 2020.

On the correlation between a sub-level qualifier refining the danger level with observations and models relating to the contributing factors of avalanche danger, Techel et al., 2022.

Today (28.11.) also a livestream on the topic:

This article has been automatically translated by DeepL with subsequent editing. If you notice any spelling or grammatical errors or if the translation has lost its meaning, please write an e-mail to the editors.

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