Auflistung Fakultät für Bauingenieurwesen und Geodäsie nach Autor/in "d2c223c9-933d-4c5c-bb98-6d9584942519"

Auflistung Fakultät für Bauingenieurwesen und Geodäsie nach Autor/in "d2c223c9-933d-4c5c-bb98-6d9584942519"

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  • Tarasova, Larisa; Merz, Ralf; Kiss, Andrea; Basso, Stefano; Blöschl, Guenter; Merz, Bruno; Viglione, Alberto; Plötner, Stefan; Guse, Björn; Schumann, Andreas; Fischer, Svenja; Ahrens, Bodo; Anwar, Faizan; Bárdossy, András; Bühler, Philipp; Haberlandt, Uwe; Kreibich, Heidi; Krug, Amelie; Lun, David; Mueller-Thomy, Hannes; Pidoto, Ross; Primo, Cristina; Seidel, Jochen; Vorogushyn, Sergiy; Wietzke, Luzie (Hoboken, NJ : Wiley-Blackwell, 2019)
    A wide variety of processes controls the time of occurrence, duration, extent, and severity of river floods. Classifying flood events by their causative processes may assist in enhancing the accuracy of local and regional ...
  • Plötner, Stefan; Haberlandt, Uwe (München : European Geosciences Union, 2016)
    The index-flood method has become the standard method for peak flow regionalisation of given return periods at ungauged basins. Moreover grouping stations into regions of homogeneous flood characteristics increases the ...
  • Krysanova, Valentina; Vetter, Tobias; Eisner, Stephanie; Huang, Shaochun; Pechlivanidis, Ilias; Strauch, Michael; Gelfan, Alexander; Kumar, Rohini; Aich, Valentin; Arheimer, Berit; Chamorro, Alejandro; van Griensven, Ann; Kundu, Dipangkar; Lobanova, Anastasia; Mishra, Vimal; Plötner, Stefan; Reinhardt, Julia; Seidou, Ousmane; Wang, Xiaoyan; Wortmann, Michel; Zeng, Xiaofan; Hattermann, Fred F. (Bristol : Institute of Physics Publishing, 2017)
    An intercomparison of climate change impacts projected by nine regional-scale hydrological models for 12 large river basins on all continents was performed, and sources of uncertainty were quantified in the framework of ...
  • Plötner, Stefan; Haberlandt, Uwe; Petry, Uwe (München : European Geosciences Union, 2017)
    In order to project changes in flood flows climate change factors can be used. These are estimated by hydrological modelling for future and historical conditions, deriving flood peak distributions each and calculating ...

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