Articles | Volume 24, issue 2
https://doi.org/10.5194/hess-24-771-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-771-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The impact of initial conditions on convection-permitting simulations of a flood event over complex mountainous terrain
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Marie Pontoppidan
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Stefan Sobolowski
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen, Norway
Alfonso Senatore
Department of Environmental Engineering, University of Calabria, Arcavacata di Rende (CS), Italy
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18 citations as recorded by crossref.
- A coupled PSR-based framework for holistic modeling and flood resilience assessment: A case study of the 2022 flood events in five southern provinces of China X. Fu et al. 10.1016/j.jhydrol.2024.131255
- Meteorological–hydrological coupling flood forecast and error propagation characteristics based on radar data assimilation in small- to medium sized River Basin: a case study of Zhanghe River Basin in China Y. Gao et al. 10.1007/s11069-024-06944-z
- Modelling Flash Floods Driven by Rain-on-Snow Events Using Rain-on-Grid Technique in the Hydrodynamic Model TELEMAC-2D N. Godara et al. 10.3390/w15223945
- Regional climate response to land cover change in tropical West Africa: a numerical sensitivity experiment with ESA land cover data and advanced WRF-Hydro E. Mortey et al. 10.3389/frwa.2024.1372333
- Reconstructing Flood Events in Mediterranean Coastal Areas Using Different Reanalyses and High-Resolution Meteorological Models A. Senatore et al. 10.1175/JHM-D-19-0270.1
- To develop a progressive multimetric configuration optimisation method for WRF simulations of extreme rainfall events over Egypt Y. Liu et al. 10.1016/j.jhydrol.2021.126237
- Comparison of two hydrodynamic models for their rain-on-grid technique to simulate flash floods in steep catchment N. Godara et al. 10.3389/frwa.2024.1384205
- Implementation of WRF-Hydro at two drainage basins in the region of Attica, Greece, for operational flood forecasting E. Galanaki et al. 10.5194/nhess-21-1983-2021
- Impact on discharge modelling using different spatial and temporal resolution scenarios in South of Chile I. Fustos et al. 10.1016/j.jsames.2022.103727
- Google Earth Engine-based mapping of land use and land cover for weather forecast models using Landsat 8 imagery M. Ganjirad & H. Bagheri 10.1016/j.ecoinf.2024.102498
- Potential contribution of land cover change on flood events in the Senegal River basin A. Ndiaye et al. 10.3389/frwa.2024.1447577
- Quantifying the sources of uncertainty for hydrological predictions with WRF-Hydro over the snow-covered region in the Upper Indus Basin, Pakistan M. Shafqat Mehboob et al. 10.1016/j.jhydrol.2022.128500
- Lateral terrestrial water flow contribution to summer precipitation at continental scale – A comparison between Europe and West Africa with WRF‐Hydro‐tag ensembles J. Arnault et al. 10.1002/hyp.14183
- Impact of Fully Coupled Hydrology-Atmosphere Processes on Atmosphere Conditions: Investigating the Performance of the WRF-Hydro Model in the Three River Source Region on the Tibetan Plateau, China G. Li et al. 10.3390/w13233409
- Convection‐permitting modeling with regional climate models: Latest developments and next steps P. Lucas‐Picher et al. 10.1002/wcc.731
- Hydrometeorological Ensemble Forecast of a Highly Localized Convective Event in the Mediterranean L. Furnari et al. 10.3390/w12061545
- Understanding the role of initial soil moisture and precipitation magnitude in flood forecast using a hydrometeorological modelling system D. Yin et al. 10.1002/hyp.14710
- Regional water cycle sensitivity to afforestation: synthetic numerical experiments for tropical Africa J. Arnault et al. 10.3389/fclim.2023.1233536
Latest update: 22 Nov 2024
Short summary
We assessed the impact of initial conditions on convection-permitting simulations of a flood event over mountainous terrain. The calibrated convection-permitting model performs better than the simpler conceptual model. Discharge is slightly more sensitive to spin-up time than precipitation due to the influence of soil moisture. A maximum of 0.5 m of snow is converted to runoff irrespective of the initial snow depth, and this snowmelt contributes to discharge mostly during peak flow period.
We assessed the impact of initial conditions on convection-permitting simulations of a flood...