PG: You have been working at the WSL Institute for Snow and Avalanche Research SLF since 2009 and as an avalanche forecaster in avalanche warning since the winter of 2010. Now you have completed your doctoral thesis in fall 2020 with the title: "On consistency and quality in public avalanche forecasting - a data-driven approach to forecast verification and to refining definitions of avalanche danger" (pdf download). What exactly is your dissertation about?
FT: On the one hand, I looked at the question of how good the quality of the avalanche forecast is, in particular the quality of the hazard level issued. So I investigated the question: was the forecast right or wrong? The answer to this question is very relevant - for avalanche forecasters to recognize where the forecast needs to be improved in the long term, and of course also as a reference point for ski tourers and freeriders who use the forecasts. But unfortunately, answering this question is also very difficult, as a danger level is not something that can be measured. This means that even when checking a forecast, a classification is made by a human being and uncertainties remain.
In addition, I compared the forecast products of the avalanche warning services in the Alpine region. In addition to the issued danger level, I was also interested in whether there are differences and similarities in the content and presentation of the forecast.
PG: What were your results? How good is the issued danger level?
In Switzerland, I evaluated the feedback from trained observers after a day in the field and compared it with the issued danger level. Taking into account the dispersion of the feedback on the same day in the same region, it turned out that on about six out of seven days the forecast was assessed as correct, on one day as too high, and almost never as too low. I also found very similar results for Norway, Canada and Colorado.
PG: And the comparison of neighboring warning services in the Alpine region. Have you noticed any differences?
Yes, I have noticed some major differences, particularly in the hazard level issued. For example, danger level 4 (major) was used much more frequently in France and parts of Italy than in Switzerland or Austria, for example. On the other hand, it was also found that on the same day, the hazard level varied by one level on average on a third of the days across warning service boundaries. It is of course clear that differences between neighboring regions are to be expected if the topography and snow climate differ. If, for example, the main Alpine ridge lies between two neighboring warning regions, such as between Valais (CH) and Valle d'Aosta (IT), then differences are to be expected. In contrast, differences in neighboring regions, such as between Samnaun (CH) and Ischgl (AT) or between Ticino (CH) and the neighboring regions in Lombardy and Piedmont, should be rarer. However, differences in the hazard level issued between these regions were also observed quite frequently in some cases.