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Application of a hydrological-hydraulic modelling cascade in lowlands for investigating water and sediment fluxes in catchment, channel and reach Cover

Application of a hydrological-hydraulic modelling cascade in lowlands for investigating water and sediment fluxes in catchment, channel and reach

Open Access
|Dec 2013

Abstract

This study shows a comprehensive simulation of water and sediment fluxes from the catchment to the reach scale. We describe the application of a modelling cascade in a well researched study catchment through connecting stateof- the-art public domain models in ArcGIS. Three models are used consecutively: (1) the hydrological model SWAT to evaluate water balances, sediment input from fields and tile drains as a function of catchment characteristics; (2) the onedimensional hydraulic model HEC-RAS to depict channel erosion and sedimentation along a 9 km channel onedimensionally; and (3) the two-dimensional hydraulic model AdH for simulating detailed substrate changes in a 230 m long reach section over the course of one year. Model performance for the water fluxes is very good, sediment fluxes and substrate changes are simulated with good agreement to observed data. Improvement of tile drain sediment load, simulation of different substrate deposition events and carrying out data sensitivity tests are suggested as future work. Main advantages that can be deduced from this study are separate representation of field, drain and bank erosion processes; shown adaptability to lowland catchments and transferability to other catchments; usability of the model’s output for habitat assessments.

DOI: https://doi.org/10.2478/johh-2013-0042 | Journal eISSN: 1338-4333 | Journal ISSN: 0042-790X
Language: English
Page range: 334 - 346
Published on: Dec 1, 2013
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year

© 2013 Jens Kiesel, Britta Schmalz, Gary L. Brown, Nicola Fohrer, published by Slovak Academy of Sciences, Institute of Hydrology
This work is licensed under the Creative Commons License.