Search results for "Sinuosity"

showing 4 items of 4 documents

The effect of geometrical parameters on the discharge capacity of meandering compound channels

2008

A number of methods and formulae has been proposed in the literature to estimate the discharge capacity of compound channels. When the main channel has a meandering pattern, a reduction in the conveyance capacity for a given stage is observed, which is due to the energy dissipations caused by the development of strong secondary currents and to the decrease of the main channel bed slope with respect to the valley bed slope. The discharges in meandering compound channels are usually assessed applying, with some adjustments, the same methods used in the straight compound channels. Specifically, the sinuosity of the main channel is frequently introduced to account for its meandering pattern, al…

Compound channels Meanders Sinuosity Stage—discharge curves Numerical simulationHydrologyMean curvatureComputer simulationTurbulenceGeometrySinuosityRadiusDissipationSettore ICAR/01 - IdraulicaReynolds-averaged Navier–Stokes equationsGeologyComputer Science::Information TheoryWater Science and TechnologyCommunication channelAdvances in Water Resources
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Testing the use of an image-based technique to measure gully erosion at Sparacia experimental area

2016

The first part of this investigation was aimed at testing the use of a three-dimensional (3D) Digital Terrain Model (DTM) and a quasi-tridimensional (2.5D) Digital Elevation Model (DEM) obtained by a large series of oblique images of eroded channels taken from consumer un-calibrated and non-metric cameras. For two closed earth channels having a different sinuosity the ground measurement of some cross-sections by a profilometer (P) was carried out. The real volume of each channel was also measured by waterproofing it by a plastic film and filling it with a known volume of water. The comparison among the three methods (3D, 2.5D and P) pointed out that a limited underestimation of the total vo…

010504 meteorology & atmospheric sciencesSoil scienceChannelized04 agricultural and veterinary sciencesSinuosity01 natural sciencesVolume (thermodynamics)040103 agronomy & agricultureErosion0401 agriculture forestry and fisheriesProfilometerEmpirical relationshipDigital elevation modelGeology0105 earth and related environmental sciencesWater Science and TechnologyRemote sensingCommunication channelHydrological Processes
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Simplified Probabilistic-Topologic Model for Reproducing Hillslope Rill Network Surface Runoff

2015

AbstractThis work presents a simplified probabilistic-topologic model for reproducing rill network surface runoff on a square-plane hillslope. The model requires only two parameters: the first is related to the production capacity of overland flow of the hillslope, at the initial conditions of the process, and the second depends on the sinuosity of the rill network. From a hydrological point of view, the following parameters account for the effects that essentially delineate the hydrologic response of a natural hillslope: rainfall intensity, hillslope roughness, and slope. Obviously, the reliability of the model is pending experimental validation that has only just begun. However, a prelimi…

Hydrologygeographygeography.geographical_feature_categoryProbabilistic logicSurface finishSinuosityExperimental validationAgricultural and Biological Sciences (miscellaneous)RillHydrology (agriculture)Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSurface runoffsurface runoff cellular automata hillslopeGeologyIntensity (heat transfer)Water Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Effects of hydrological events on morphological evolution of a fluvial system

2018

Abstract This study quantifies morphological evolution of the Dez River, Iran, from 1955 to 2016. The approach uses a sequence of Landsat images, aerial photos, and topographic maps. In addition, the hydrological data including average daily discharge and yearly maximum discharge at the Dezful hydrological station for the period (1955–2016) were used. The study reach was divided into 48 meander loops from upstream to downstream. Active channel width (w) was determined at 10 m intervals and changes assessed along the study reach of the Dez River. Morphological indices including sinuosity index; straight meander length; centerline flow length; erosion area; erodible length channel migration; …

Return periodFlood magnitude010504 meteorology & atmospheric sciencesChannel widthCutoffSinuosity010502 geochemistry & geophysics01 natural sciencesHydrology (agriculture)Satellite imagery0105 earth and related environmental sciencesWater Science and TechnologyEcologia fluvialFlood frequencyHydrologygeographySinuositygeography.geographical_feature_categoryFlood mythPE&RCChannel plan-formMeander bendErosionMeanderGeologyChannel (geography)
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