Abstract
This review paper investigates the determinants of modelling choices, for numerous applications of 1-D free-surface flow and morphodynamic equations in hydrology and hydraulics, across multiple spatiotemporal scales. We aim to characterize each case study by its signature composed of model refinement (Navier-Stokes: NS; Reynolds-averaged Navier-Stokes: RANS; Saint-Venant: SV; or approximations to Saint-Venant: ASV), spatiotemporal scales and subscales (domain length: L from 1ĝ€cm to 1000ĝ€km; temporal scale: T from 1ĝ€s to 1 year; flow depth: H from 1ĝ€mm to 10ĝ€m; spatial step for modelling: δ L; temporal step: δ T), flow typology (Overland: O; High gradient: Hg; Bedforms: B; Fluvial: F), and dimensionless numbers (dimensionless time period T ∗, Reynolds number Re, Froude number Fr, slope S, inundation ratio z, Shields number θ). The determinants of modelling choices are therefore sought in the interplay between flow characteristics and cross-scale and scale-independent views. The influence of spatiotemporal scales on modelling choices is first quantified through the expected correlation between increasing scales and decreasing model refinements (though modelling objectives also show through the chosen spatial and temporal subscales). Then flow typology appears a secondary but important determinant in the choice of model refinement. This finding is confirmed by the discriminating values of several dimensionless numbers, which prove preferential associations between model refinements and flow typologies. This review is intended to help modellers in positioning their choices with respect to the most frequent practices, within a generic, normative procedure possibly enriched by the community for a larger, comprehensive and updated image of modelling strategies.
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CITATION STYLE
Cheviron, B., & Moussa, R. (2016, September 14). Determinants of modelling choices for 1-D free-surface flow and morphodynamics in hydrology and hydraulics: A review. Hydrology and Earth System Sciences. Copernicus GmbH. https://doi.org/10.5194/hess-20-3799-2016
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