Search results for " rating curve"

showing 4 items of 4 documents

Unsteady State Water Level Analysis for Discharge Hydrograph Estimation in Rivers with Torrential Regime: The Case Study of the February 2016 Flood E…

2017

Discharge hydrograph estimation during floods, in rivers with torrential regime, is often based on the use of rating curves extrapolated from very low stage-discharge measurements. To get a more reliable estimation, a reverse flow routing problem is solved using water level data measured in two gauged stations several kilometers from each other. Validation of the previous analysis carried out on the flood event of February 2016 at the Europa Bridge and Castiglione Scalo sections of the Crati River (Cosenza, Italy) is based on the use of 'soft' discharge measurement data and the comparison of the water level data computed in the downstream gauged section by three different hydraulic models w…

EstimationHydrologyrating curveFlood mythMeteorologyDiffusive model0208 environmental biotechnologyGeography Planning and DevelopmentHydrographdischarge estimation02 engineering and technologyfloodAquatic ScienceBiochemistrySettore ICAR/01 - Idraulica020801 environmental engineeringWater levelPeak flowreverse routing; rating curves; diffusive model; peak flow; discharge estimation; floodEnvironmental scienceReverse routingFlow routingWater Science and TechnologyEvent (probability theory)Water
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Discussion of “Unsteady Stage-Discharge Relationships for Sharp-Crested Weirs” by Firouz Ghasemzadeh, Salah Kouchakzadeh, and Gilles Belaud

2021

I would like to thank the authors for writing this interesting article dealing with unsteady stage-discharge relationships for sharp-crested weirs. The operation of triangular and rectangular sharp-crested weirs in unsteady flow conditions was experimentally investigated. Results indicated the presence of looped rating curves, with transposition of the rising and falling limbs compared to that commonly observed in stream gauge ratings. The authors found that the deviation between steady and unsteady flow rates in the looped rating curves depends on the weir type and the hydrograph gradient (i.e., the temporal depth variation), especially when the latter changes rapidly. Finally, they propos…

HydrologySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliStage (hydrology)Agricultural and Biological Sciences (miscellaneous)complex rating curves rectangular and triangular weirs analytical solution unsteady state stage-discharge relationshipsGeologyWater Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Complex Rating Curves for Sharp Crested Orifices and Rectangular or Triangular Weirs under Unsteady Flow Conditions

2021

The importance of discharge measurements is fully acknowledged in many research fields, mostly in hydrology. Numerous measurement devices and various overflow structures have been proposed for discharge measurements; however, their use is based on calibrated simple stage discharge relationships that may cause significant errors when unsteady flow conditions occur. This issue is quite common because of rainfall and runoff temporal variability that inhibits the achievement of the steady state. Although this issue has already been experimentally investigated, it seems that a physically based line of approach has not been attempted before. In this paper, unsteady stage discharge relationships o…

Unsteady flowHydrology (agriculture)Discharge measurementsEnvironmental ChemistrySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliMechanicsGeologyBody orificeComplex rating curves sharp crested orifice rectangular and triangular weirs stage-discharge relationshipGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
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Computation of vertically averaged velocities in irregular sections of straight channels

2015

Abstract. Two new methods for vertically averaged velocity computation are presented, validated and compared with other available formulas. The first method derives from the well-known Huthoff algorithm, which is first shown to be dependent on the way the river cross section is discretized into several subsections. The second method assumes the vertically averaged longitudinal velocity to be a function only of the friction factor and of the so-called "local hydraulic radius", computed as the ratio between the integral of the elementary areas around a given vertical and the integral of the elementary solid boundaries around the same vertical. Both integrals are weighted with a linear shape f…

lcsh:GE1-350diffusive modeldischarge estimation irregular section rating curve uniform flow.Discretizationlcsh:TComputationlcsh:Geography. Anthropology. RecreationGeometryHydrographRadiusRating curveFunction (mathematics)lcsh:Technologylcsh:TD1-1066Settore ICAR/01 - IdraulicaCross section (physics)lcsh:GPotential flowlcsh:Environmental technology. Sanitary engineeringlcsh:Environmental sciencesMathematics
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