Gastwissenschafter, SLF Davos, WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260 Davos Dorf
These snow projections will use the Klima CH2025 bias-adjusted GCM-RCM model runs
A recently discovered process of airborne snow metamorphism (ASM) affects the storage of isotope climate signals in ice sheets and the energy and mass balance of polar regions.
cold lab experiments, implementing ASM into the coupled atmosphere-snow cover model
We analyse the stability of Lotka-Volterra competition models
Lotka-Volterra competition model ¶ \( \frac{dx_i}{dt}= x_i r_i (1- \frac{ \sum
Rheinblick2027 investigates the effects of climate change on the Rhine River discharge based on the latest state-of-the-art.
We will further investigate hydrological model comparisons, including previous streamflow
Phenology might not be only controlled by temperature, photoperiod and water availability but also by tree intrinsic factors related to sink-source relationships.
on senescence progression, and embed the detected mechanisms into a phenology model
The rock slope instability „Spitze Stei“ constitutes a risk for the touristic infrastructure around lake Öschinensee and the village Kandersteg. Our project task will investigate the mechanisms which led to the slope destabilisation and analyse scenarios for slope failures.
We want to apply a thermo-mechanical model, which is fed with the rock-mechanical
The environmental, social and economic impacts of feeding the Swiss population are immense, and largely fall outside of Swiss borders. New, harmonized and transdisciplinary methods are needed to track these multidimensional impacts to support new dialogues between science, society and policy in orde
In parallel, we will (iv) develop a model of the entire Swiss agri-food system to
Gastwissenschafter, WSL Birmensdorf, Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf
J.W. (2015): Calculation of bedload transport in Swiss mountain rivers using the model
Software Engineer, SLF Davos, WSL-Institut für Schnee- und Lawinenforschung SLF, Flüelastrasse 11, 7260 Davos Dorf
These models include the multi-layer, energy balance snow model SNOWPACK, the Alpine
Most investigations use models and thus require climate forcing data.
change signal as diagnosed in CH-2018 will be superimposed on regional weather model
