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Peer-reviewedCC BY 4.0Natural Hazards and Earth System Sciences

Towards improved integration of hydrological uncertainty and hydraulic model sensitivity in flood hazard mapping

  1. 1University of Ljubljana (Ljubljana, Slovenia)

Abstract

The study presents a novel framework for integrating hydrological uncertainties and the related sensitivity of the hydrodynamic modelling results into flood hazard mapping. Uncertainties in flood frequency analysis (FFA), including anticipated impact of climate change and sensitivity to channel and floodplain roughness, were examined through selected scenario ensembles. The study area is the lower Vipava river, a transboundary catchment shared between Slovenia and Italy with variable floodplain topography. Sensitivity analysis revealed that uncertainty in FFA and river channel roughness significantly influenced the inundation spatial extent and inundation depth, the impact of floodplain roughness appears to be limited. The analysis shows that natural successional changes in river channel roughness substantially impact the results of a 10 year return period (RP) event, increasing flood extent by 45 %. The increase in inundated areas is less pronounced for 100 and 500 year RP floods, with increases of 15 % and 11 %, respectively. The weighted exceedance probability of inundation (WEPI) based on scenario ensembles provided an informative identification of areas most susceptible to potential changes in flood hazard. Our results highlight the value of targeted scenario ensembles that incorporate FFA uncertainty and hydraulic roughness sensitivity, thereby producing more informative flood hazard mapping that can complement deterministic mapping approaches and support more adaptive future land use planning.

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BibTeX
@article{rusjan2026towards,
  title = {{Towards improved integration of hydrological uncertainty and hydraulic model sensitivity in flood hazard mapping}},
  author = {Simon Rusjan and Jasna Donevska and Matjaž Mikoš},
  journal = {Natural Hazards and Earth System Sciences},
  year = {2026},
  month = nov,
  doi = {10.5194/nhess-26-5647-2026},
  url = {https://nhess.copernicus.org/articles/26/5647/2026/},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Towards improved integration of hydrological uncertainty and hydraulic model sensitivity in flood hazard mapping
AU  - Simon Rusjan
AU  - Jasna Donevska
AU  - Matjaž Mikoš
PY  - 2026
DA  - 2026/11/05
JO  - Natural Hazards and Earth System Sciences
DO  - 10.5194/nhess-26-5647-2026
UR  - https://nhess.copernicus.org/articles/26/5647/2026/
AB  - The study presents a novel framework for integrating hydrological uncertainties and the related sensitivity of the hydrodynamic modelling results into flood hazard mapping. Uncertainties in flood frequency analysis (FFA), including anticipated impact of climate change and sensitivity to channel and floodplain roughness, were examined through selected scenario ensembles. The study area is the lower Vipava river, a transboundary catchment shared between Slovenia and Italy with variable floodplain topography. Sensitivity analysis revealed that uncertainty in FFA and river channel roughness significantly influenced the inundation spatial extent and inundation depth, the impact of floodplain roughness appears to be limited. The analysis shows that natural successional changes in river channel roughness substantially impact the results of a 10 year return period (RP) event, increasing flood extent by 45 %. The increase in inundated areas is less pronounced for 100 and 500 year RP floods, with increases of 15 % and 11 %, respectively. The weighted exceedance probability of inundation (WEPI) based on scenario ensembles provided an informative identification of areas most susceptible to potential changes in flood hazard. Our results highlight the value of targeted scenario ensembles that incorporate FFA uncertainty and hydraulic roughness sensitivity, thereby producing more informative flood hazard mapping that can complement deterministic mapping approaches and support more adaptive future land use planning.
SN  - 1684-9981
ER  -