Bettina Schaefli, you’re a pioneer when it comes to modelling Alpine water resources. Why is that?
I fell into it, so to speak. For my doctoral thesis, I did the first study on future hydropower in the Swiss Alps. Of course, there were already some model-based approaches, but my study was the first to take the results of climate model runs into account and that tried to estimate uncertainties with regard to water resources in the Alps. I started at the beginning of the 2000s, when a new era of climate change impact simulation started, using several models and scenarios. This ultimately influenced my specialization in long-term prediction for water resources. My focus is still strongly on Alpine water resources, but I have also diversified. For example, a recently completed doctoral thesis dealt with the water resources in Volta River basin in Africa. Of course, this poses completely different modelling challenges than in Switzerland, where we have a good data basis.
In the future, Switzerland will be confronted with seasonal and local water scarcity. How well can you create models for these situations?
This will be one of my future research priorities. Among other things, I’m interested in how technical irrigation options, which are always being developed in agriculture, could lead to water scarcity. This involves small catchment areas across the Swiss Plateau. This region will be much more affected by water scarcity than the Alps, and it will lead to interesting questions.
Are such small-scale climate impacts more difficult to model than large-scale changes?
In terms of precision, some very different challenges arise. If we’re in a mountain catchment area where precipitation can’t be measured accurately, even a 20 percent margin of error is still acceptable. On the other hand, if we move into Swiss Plateau catchment areas that are used for agricultural purposes, the requirements are completely different. Small-scale modelling makes it more difficult to scale down climate model runs, but the meteorological conditions of the Swiss Plateau are less heterogeneous than in the Alps.