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Number of items: 10.

Staudinger, Maria; Stoelzle, Michael; Cochand, Fabien; Seibert, Jan; Weiler, Markus; Hunkeler, Daniel (2019). Your work is my boundary condition!: Challenges and approaches for a closer collaboration between hydrologists and hydrogeologists. Journal of Hydrology, 571:235-243.

Jenicek, Michal; Seibert, Jan; Staudinger, Maria (2018). Modeling of future changes in seasonal snowpack and impacts on summer low flows in alpine catchments. Water Resources Research, 54(1):538-556.

Staudinger, Maria; Stoelzle, Michael; Seeger, Stefan; Seibert, Jan; Weiler, Markus; Stahl, Kerstin (2017). Catchment water storage variation with elevation. Hydrological Processes, 31(11):2000-2015.

Jeníček, Michal; Seibert, Jan; Zappa, Massimiliano; Staudinger, Maria; Jonas, Tobias (2016). Importance of maximum snow accumulation for summer low flows in humid catchments. Hydrology and Earth System Sciences, 20(2):859-874.

Staudinger, Maria. Characterization and predictability of low flows based on conceptual modeling. 2015, University of Zurich, Faculty of Science.

Orth, Rene; Staudinger, Maria; Seneviratne, Sonia I; Seibert, Jan; Zappa, Massimiliano (2015). Does model performance improve with complexity? A case study with three hydrological models. Journal of Hydrology, 523:147-159.

Staudinger, Maria; Weiler, Markus; Seibert, Jan (2015). Quantifying sensitivity to droughts – an experimental modeling approach. Hydrology and Earth System Sciences, 19(3):1371-1384.

Staudinger, Maria; Stahl, Kerstin; Seibert, Jan (2014). A drought index accounting for snow. Water Resources Research, 50(10):7861-7872.

Staudinger, Maria; Seibert, Jan (2014). Predictability of low flow – An assessment with simulation experiments. Journal of Hydrology, 519:1383-1393.

Staudinger, Maria; Stahl, K; Seibert, Jan; Clark, M P; Tallaksen, L M (2011). Comparison of hydrological model structures based on recession and low flow simulations. Hydrology and Earth System Sciences, 15(11):3447-3459.

This list was generated on Mon Aug 19 02:20:26 2019 CEST.