Search results for "Shallow Water"

showing 10 items of 74 documents

Finite-Element Modeling of Floodplain Flow

2000

A new methodology for a robust solution of the diffusive shallow water equations is proposed. The methodology splits the unknowns of the momentum and continuity equations into one kinematic and one parabolic component. The kinematic component is solved using the slope of the water level surface computed in the previous time-step and a zero-order approximation of the water head inside the mass-balance area around each node of the mesh. The parabolic component is found by applying a standard finite-element Galerkin procedure, where the source terms can be computed from the solution of the previous kinematic problem. A simple 1D case, with a known analytical solution, is used to test the accur…

Hydrologyshallow-water equationComputer simulationWater flowMechanical EngineeringMathematical analysisKinematicsFinite element methodfinite element analysiHydraulic headflood flowFlow (mathematics)flood plainGalerkin methodShallow water equationsWater Science and TechnologyCivil and Structural EngineeringMathematics
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Long time behavior for a dissipative shallow water model

2013

We consider the two-dimensional shallow water model derived by Levermore and Sammartino (Nonlinearity 14,2001), describing the motion of an incompressible fluid, confined in a shallow basin, with varying bottom topography. We construct the approximate inertial manifolds for the associated dynamical system and estimate its order. Finally, considering the whole domain R^2 and under suitable conditions on the time dependent forcing term, we prove the L^2 asymptotic decay of the weak solutions.

Inertial frame of referenceFourier splitting methodDynamical Systems (math.DS)Space (mathematics)Dynamical system01 natural sciencesPhysics::Fluid DynamicsNavier–Stokes equationsMathematics - Analysis of PDEsAttractorFOS: MathematicsMathematics - Dynamical Systems0101 mathematicsNavier–Stokes equationsPhysics::Atmospheric and Oceanic PhysicsMathematical PhysicsMathematicsApplied Mathematics010102 general mathematicsMathematical analysisAttractorIncompressible viscous fluidInertial manifoldFunctional Analysis (math.FA)Mathematics - Functional Analysis010101 applied mathematicsWaves and shallow waterTime decayDissipative systemCompressibilityAnalysisAnalysis of PDEs (math.AP)Annales de l'Institut Henri Poincaré C, Analyse non linéaire
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Diffusive Modeling of Aggradation and Degradation in Artificial Channels

2008

The unsteady flow and solid transport simulation problem in artificial channels is solved using a three-equation model, coupled with a local erosion law. The three equations are the water mass and momentum balance equations, as well as the total solid load balance equation. It is shown that even during severe hydrological events inertial terms can be neglected in the momentum equation without any substantial change in the solution sought. Empirical equilibrium formulas were used to estimate the solid load as a function of the flow variables. Local erosion, due to the scour generated at the jump between two channels connected at different bottom elevations, was estimated adapting a literatur…

Inertial frame of referenceSpacetimeMechanical EngineeringFunction (mathematics)MechanicsSettore ICAR/01 - IdraulicaOpen-channel flowFlow (mathematics)JumpGeotechnical engineeringDiffusion (business)sediment transport shallow waters solid load unsteady flow numerical models local scourSediment transportWater Science and TechnologyCivil and Structural EngineeringMathematicsJournal of Hydraulic Engineering
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Lower and Middle Cambrian brachiopods from the Iberian Chains and Sierra Morena (Spain)

2021

Brachiopods from the Lower and Middle Cambrian of the Iberian Chains and Sierra Morena are described. The following taxa occur in the Iberian Chains: "Lingulella" sp., Redlichella cf. bohemica (Barrande), Dictyonina radioplicata sp. n., Micromitra sp., Trematobolus simplex (Vogel), Trematobolus borobiensis sp. n. and Jamesella sp. The taxa "Lingulella" sp. and Sibiria? sp. are reported from the Lower Cambrian of Sierra Morena. Brachiopods constitute several distinct associations: the relatively shallow water Trematobolus assemblage near the Lower-Middle Cambrian boundary interval is followed by the deeper Dictyonina­Redlichella assemblage. The alternation of these assemblages permit us to i…

LingulellaPaleontologyWaves and shallow waterTaxonbiologyMicromitraPaleontologyAssemblage (archaeology)biology.organism_classificationbrachiopoda lower cambrian middle cambrian spain.QE701-760GeologySea levelSpanish Journal of Palaeontology
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A non-hydrostatic pressure distribution solver for the nonlinear shallow water equations over irregular topography

2016

Abstract We extend a recently proposed 2D depth-integrated Finite Volume solver for the nonlinear shallow water equations with non-hydrostatic pressure distribution. The proposed model is aimed at simulating both nonlinear and dispersive shallow water processes. We split the total pressure into its hydrostatic and dynamic components and solve a hydrostatic problem and a non-hydrostatic problem sequentially, in the framework of a fractional time step procedure. The dispersive properties are achieved by incorporating the non-hydrostatic pressure component in the governing equations. The governing equations are the depth-integrated continuity equation and the depth-integrated momentum equation…

Mathematical optimizationFinite volume method010504 meteorology & atmospheric sciencesDiscretization0208 environmental biotechnology02 engineering and technologyMechanicsSolver01 natural sciencesSettore ICAR/01 - Idraulica020801 environmental engineeringUnstructured gridlaw.inventionNonlinear systemContinuity equationlawDynamic pressure Shallow waters Dispersive process Finite volume Wetting and drying Unstructured gridHydrostatic equilibriumShallow water equationsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesWater Science and TechnologyMathematicsAdvances in Water Resources
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The role of topography and erosion in the development and architecture of shallow-water coral bioherms (Tortonian-Messinian, Cabo de Gata, SE Spain).

2009

23 pages; International audience; During the Miocene, Mediterranean shallow-water carbonates were rich in scleractinian corals, which thrive in various depositional settings. A Tortonian–Messinian bioherm belt developing in a heterozoan-dominated ramp was investigated along a 1.2 km continuous transect located in the Cabo de Gata region. The interval studied displays four depositional environments from mid-to-inner ramp, dominated by swell waves and storm energy, deposited as a single, large-scale depositional sequence during a 3rd to 4th order transgressive–regressive cycle. The bioherms grew in three phases, and were essentially composed of inplace primary frameworks. Three coral genera w…

Micro-encrusters010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStormsCoralPorites010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentBiohermPaleontologyStormBack-reef erosionPalaeotopography14. Life underwaterTransectEcology Evolution Behavior and SystematicsSea level0105 earth and related environmental sciencesEarth-Surface ProcessesMicro-encrustergeographygeography.geographical_feature_categorybiologyPaleontologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationWaves and shallow waterVolcano[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyErosionCoralGeology
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A new algorithm for a robust solution of the fully dynamic Saint-Venant equations

2003

A new procedure for the numerical solution of the fully dynamic shallow water equations is presented. The procedure is a fractional step methodology where the original system is split into two sequential ones. The first system differs from the original one because of the head gradient term, that is treated as constant and equal to the value computed at the end of the previous time step. The solution of this system, called kinematic, is computed in each element using a spatial zero order approximation for both the heads and the flow rates by means of integration of single ODEs. The second system is called diffusive, contains in the momentum equations only the complementary terms and can be e…

MomentumCourant–Friedrichs–Lewy conditionCalculusApplied mathematicsBoundary value problemApproxConstant (mathematics)Conservation of massShallow water equationsFlow routingWater Science and TechnologyCivil and Structural EngineeringMathematicsJournal of Hydraulic Research
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Multivariate-Analysis of Phytoplankton and Related Environmental-Factors, in a Shallow Hypertrophic Lake

1995

Data on some relevant environmental variables and phytoplankton species composition, collected from the hypertrophic shallow lake Albufera of Valencia (Spain) during 1980-88, were examined using Redundancy Analysis (RDA). The hydrological cycle of the lake is manipulated for rice cultivation in the area. Seasonality and the particular hydrological cycle of the lake were the principal factors influencing long-term phytoplankton dynamics. Annual or horizontal differences were less important than the seasonal factor. However, a trend of phosphate increase and underwater illumination decrease was observed between 1980 and 1988. These changes might be related to some species year-to-year variati…

Multivariate analysisEcologyfungiEnvironmental factorSampling (statistics)Aquatic ScienceSeasonalitymedicine.diseasemedicine.disease_causeWaves and shallow waterPhytoplanktonmedicineEnvironmental sciencePhysical geographyWater cycleEutrophicationHydrobiologia
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MAST-2D diffusive model for flood prediction on domains with triangular Delaunay unstructured meshes

2011

Abstract A new methodology for the solution of the 2D diffusive shallow water equations over Delaunay unstructured triangular meshes is presented. Before developing the new algorithm, the following question is addressed: it is worth developing and using a simplified shallow water model, when well established algorithms for the solution of the complete one do exist? The governing Partial Differential Equations are discretized using a procedure similar to the linear conforming Finite Element Galerkin scheme, with a different flux formulation and a special flux treatment that requires Delaunay triangulation but entire solution monotonicity. A simple mesh adjustment is suggested, that attains t…

Nonlinear systemMathematical optimizationDiscretizationDelaunay triangulationCourant–Friedrichs–Lewy conditionshallow waters numerical methods finite element method diffusive model unstructured meshes Delaunay triangulations Voronoi cells unsteady flow backwater effect analytical solutionLinear systemApplied mathematicsGalerkin methodShallow water equationsFinite element methodWater Science and TechnologyMathematics
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Well-balanced bicharacteristic-based scheme for multilayer shallow water flows including wet/dry fronts

2013

The aim of this paper is to present a new well-balanced finite volume scheme for two-dimensional multilayer shallow water flows including wet/dry fronts. The ideas, presented here for the two-layer model, can be generalized to a multilayer case in a straightforward way. The method developed here is constructed in the framework of the Finite Volume Evolution Galerkin (FVEG) schemes. The FVEG methods couple a finite volume formulation with evolution operators. The latter are constructed using the bicharacteristics of multidimensional hyperbolic systems. However, in the case of multilayer shallow water flows the required eigenstructure of the underlying equations is not readily available. Thus…

Numerical AnalysisMathematical optimizationFinite volume methodPhysics and Astronomy (miscellaneous)Applied MathematicsReliability (computer networking)Hyperbolic systemsComputer Science ApplicationsComputational MathematicsWaves and shallow waterModeling and SimulationScheme (mathematics)Applied mathematicsGalerkin methodMathematicsJournal of Computational Physics
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