Articles | Volume 20, issue 4
https://doi.org/10.5194/tc-20-2351-2026
https://doi.org/10.5194/tc-20-2351-2026
Research article
 | 
23 Apr 2026
Research article |  | 23 Apr 2026

Assessment of snow model uncertainty in relation to the effect of a 1 °C warming using the snow modelling framework openAMUNDSEN

Erwin Rottler, Brage Storebakken, Michael Warscher, Florian Hanzer, Elena Bertazza, and Ulrich Strasser

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Adhikari, T. R., Talchabhadel, R., Shrestha, S., Sharma, S., Aryal, D., and Pradhanang, S. M.: The evaluation of climate change impact on hydrologic processes of a mountain river basin, Theor. Appl. Climatol., 150, 749–762, https://doi.org/10.1007/s00704-022-04204-3, 2022. a
Albrich, K., Seidl, R., Rammer, W., and Thom, D.: From sink to source: changing climate and disturbance regimes could tip the 21st century carbon balance of an unmanaged mountain forest landscape, Forestry, 96, 399–409, https://doi.org/10.1093/forestry/cpac022, 2022. a
Alonso-González, E., Gutmann, E., Aalstad, K., Fayad, A., Bouchet, M., and Gascoin, S.: Snowpack dynamics in the Lebanese mountains from quasi-dynamically downscaled ERA5 reanalysis updated by assimilating remotely sensed fractional snow-covered area, Hydrol. Earth Syst. Sci., 25, 4455–4471, https://doi.org/10.5194/hess-25-4455-2021, 2021. a
Bair, E. H., Stillinger, T., and Dozier, J.: Snow Property Inversion From Remote Sensing (SPIReS): A Generalized Multispectral Unmixing Approach With Examples From MODIS and Landsat 8 OLI, IEEE T. Geosci. Remote, 59, 7270–7284, https://doi.org/10.1109/TGRS.2020.3040328, 2021. a
Ban, N., Caillaud, C., Coppola, E., et al.: The first multi-model ensemble of regional climate simulations at kilometer-scale resolution, part I: evaluation of precipitation, Clim. Dynam., 57, 275–302, https://doi.org/10.1007/s00382-021-05708-w, 2021. a, b
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Short summary
In this study, we simulate the snow cover in a complex mountain area under historical conditions and for a time period characterized by a 1 °C warming using a large number of different snow models. Our objective is the assessment of differences in the modelling results induced by different snow model configurations. We find that differences stemming from the choice of snowmelt method, land cover map and spatial resolution can be comparable in magnitude to the effect of a 1°C warming.
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