I travel from summery Innsbruck to Zermatt in late winter. There's supposed to be endless snow there this season. Long, lonely drives are great. At least that's what I think. They are usually characterized by an extensive journey of thought. This makes me look forward to the journey as much as the upcoming ski tours and I leave Innsbruck heading west. On the Arlberg, I am already lost in the north face of the Lyskamm, when I hear an interview on the radio about a fatal avalanche accident. The following comes out of the loudspeaker: "The people involved were on a slope steeper than 35° at avalanche warning level 3, an absolute no-go." It snaps me out of my even steeper firn dreams and transports me to another world.
Every time its current, every current its progress
As in science and art, there are and have been different eras and currents in relation to snow and how people deal with it - after all, this is also science and/or art, depending on your point of view. Some of these trends exist side by side, others merge into one another. Each one has brought about improvements - in the case of snow, most notably the emergence of probability-based decision-making strategies in the 1990s. For the past 20 years, however, this trend seems to have stalled: The same system has been reinventing itself over and over again since then - without any fundamental changes, aiming past the people themselves and no longer improving the quality of decision-making in the terrain. But let's take a closer look at the history of avalanche prevention:
The antiquity of snow & avalanche science | First half of the 20th century
When ski pioneer Mathias Zdarsky first described sublimation in relation to the snowpack in 1916, he certainly had no idea that he was laying the foundations for the application of a science that today continues to influence millions of snow-loving skiers. At the latest when Welzenbach and Paulcke took a closer look at floating snow and its connections for activity in the winter mountains around 1930, knowledge about the constructive transformation, i.e. the formation of weak layers, became acceptable and could be put into practice in the terrain for the first time. There was a fundamental understanding of what was happening in the snow and what this knowledge could be used for.
The Middle Ages | The time before Munter
Until the 1990s, little changed in the practical implementation of this knowledge, although the physical understanding of snow and avalanches improved continuously. The system was sluggish, not very innovative and mainly clung to the representative snow profile for individual slope assessment. Not a pleasant development, as was later discovered. But thankfully, the Middle Ages were eventually replaced.