Search results for "shallow water"

showing 10 items of 74 documents

Filtration pressure by bivalves affects the trophic conditions in Mediterranean shallow ecosystems

2009

Bivalve filtration may control the amount of seston in coastal waters, reducing local euthrophication and keeping degrading phenomena like hypoxia and anthropogenic pollution under control. Two Sicilian brackish-marine ponds (Ganzirri and Faro) present us with the opportunity to gain data on the effect of bivalve filtration on the amount of particulate organic matter in the field. The cultivation of bivalves has been carried out in both of the ponds since the early 1990s but stopped in Ganzirri in 1995.We tested whether the cessation of bivalve cultivation influenced features of organic matter available to suspension feeders (total suspended matter, its inorganic and organic fractions, chlo…

Settore BIO/07 - EcologiaChlorophyll abivalvesBiologybivalvechemistry.chemical_compoundMediterranean SeaEcosystemOrganic matterparticulate organic matterEcology Evolution Behavior and SystematicsGeneral Environmental ScienceTrophic levelfiltrationchemistry.chemical_classificationshallow watersEcologyEcologySestonshallow waterHypoxia (environmental)Bivalviabiology.organism_classificationchemistrybivalves; filtration; particulate organic matter; shallow waters; primary production; Mediterranean SeaGeneral Earth and Planetary SciencesEutrophicationprimary productionChemistry and Ecology
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Linking the effects of the Global Change to biodiversity and ecosystem services in shallow waters

2010

Settore BIO/07 - EcologiaGlobal change biodiversity shallow waters goods services
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The genus Ruppia L. (Ruppiaceae) in the Mediterranean region: An overview

2015

Abstract This paper reviews the current knowledge on the diversity, distribution and ecology of the genus Ruppia L. in the Mediterranean region. The genus Ruppia, a cosmopolitan aquatic plant complex, is generally restricted to shallow waters such as coastal lagoons and brackish habitats characterized by fine sediments and high salinity fluctuations. In these habitats Ruppia meadows play an important structural and functional role. Molecular analyses revealed the presence of 16 haplotypes in the Mediterranean region, one corresponding to Ruppia maritima L., and the others to various morphological forms of Ruppia cirrhosa (Petagna) Grande, all together referred to as the “R. cirrhosa s.l. co…

Settore BIO/07 - EcologiaMediterranean climateRuppiaAquatic angiospermsBrackish waterEcologySettore BIO/02 - Botanica SistematicaOverviewShallow watersPlant ScienceAquatic ScienceBiologybiology.organism_classificationRuppiaHabitatGenusAquatic plantRuppia cirrhosaBotanyAquatic angiosperms Ruppia Shallow waters Mediterranean region Overview.Mediterranean regionAquatic angiosperms Ruppia Shallow waters Mediterranean region OverviewRuppia maritimaAquatic Botany
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The shallow seagrass system in Southern Mediterranean (Sicily, Italy): a large sink of organic matter available to upper consumers.

2006

The effects of human activities related to salt production on the global complexity of a shallow hyperhaline system (Sicily, Italy) were investigated. This through monitoring dynamics of some physical, chemical and trophic factors recognised as main constraints for the origin of organic matter and its availability to apex consumers. The system was dominated by seagrass Ruppia cirrhosa and large stands of macroalga Chaetomorpha linum; isopods and gasteropods were the most abundant taxa among benthic organisms, while Aphanius fasciatus and Atherina boyeri represented up to 90% of all catch among the small resident fishes. Ruppia could function as a multidimensional framework able to increase …

Settore BIO/07 - EcologiaSeagrass Ruppia cirrhosa organic matter availability shallow waters MediterraneanSettore BIO/02 - Botanica Sistematica
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MAST solution of irrotational flow problems in 2D domains with strongly unstructured triangular meshes

2010

A new methodology for the solution of irrotational 2D flow problems in domains with strongly unstructured meshes is presented. A fractional time step procedure is applied to the original governing equations, solving consecutively a convective prediction system and a diffusive corrective system. The non linear components of the problem are concentrated in the prediction step, while the correction step leads to the solution of a linear system, of the order of the number of computational cells. A MArching in Space and Time (MAST) approach is applied for the solution of the convective prediction step. The major advantages of the model, as well as its ability to maintain the solution monotonicit…

Shallow water numerical models MASTConvectionNonlinear systemSpacetimeLinear systemApplied mathematicsMonotonic functionPolygon meshGeometryConservative vector fieldShallow water equationsSettore ICAR/01 - IdraulicaMathematicsAIP Conference Proceedings
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Un nouvel algorithme pour une solution robuste des équations complètes de Saint-Venant

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…

Shallow waterFlow routingExplicit methodCivil and Structural EngineeringWater Science and Technology
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New construction of algebro-geometric solutions to the Camassa-Holm equation and their numerical evaluation

2011

An independent derivation of solutions to the Camassa-Holm equation in terms of multi-dimensional theta functions is presented using an approach based on Fay's identities. Reality and smoothness conditions are studied for these solutions from the point of view of the topology of the underlying real hyperelliptic surface. The solutions are studied numerically for concrete examples, also in the limit where the surface degenerates to the Riemann sphere, and where solitons and cuspons appear.

Surface (mathematics)General MathematicsFOS: Physical sciencesGeneral Physics and AstronomyRiemann sphereTheta function01 natural sciences010305 fluids & plasmassymbols.namesake[MATH.MATH-MP]Mathematics [math]/Mathematical Physics [math-ph]0103 physical sciencesLimit (mathematics)0101 mathematics[MATH.MATH-MP] Mathematics [math]/Mathematical Physics [math-ph]Shallow water equationsNonlinear Sciences::Pattern Formation and SolitonsMathematical PhysicsMathematicsSmoothnessCamassa–Holm equationNonlinear Sciences - Exactly Solvable and Integrable Systems010102 general mathematicsMathematical analysisGeneral Engineering[ MATH.MATH-MP ] Mathematics [math]/Mathematical Physics [math-ph]Mathematical Physics (math-ph)Nonlinear Sciences::Exactly Solvable and Integrable SystemssymbolsExactly Solvable and Integrable Systems (nlin.SI)Hyperelliptic surfaceProc. R. Soc. Lond. Ser. A Math. Phys. Eng. Sci. 468 (2012), no. 2141, 1371–1390
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A marching in space and time solver for the complete 2D shallow water equations. Application to real test cases.

2006

Test caseSpacetimeMathematical analysisSolverShallow water equationsMathematics
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Simulation of the Propagation of Tsunamis in Coastal Regions by a Two-Dimensional Non-Hydrostatic Shallow Water Solver

2017

Due to the enormous damages and losses of human lives in the inundated regions, the simulation of the propagation of tsunamis in coastal areas has received an increasing interest of the researchers. We present a 2D depth-integrated, non- hydrostatic shallow waters solver to simulate the propagation of tsunamis, solitary waves and surges in coastal regions. We write the governing continuity and momentum equations in conservative form and discretize the domain with unstructured triangular Generalized Delaunay meshes. We apply a fractional- time-step procedure, where two problems (steps) are consecutively solved. In the first and in the second step, we hypothesize a hydrostatic and a non-hydro…

TurbulenceVoronoi cellShallow waters; Non-hydrostatic pressure; Unstructured mesh; Wetting/drying; Tsunami propagation; Long waves; Voronoi cells; Runge-Kutta method; Galerkin scheme; Manning equation; Dirichlet condition; OpenFOAMShallow waterLong waveUnstructured meshGeophysicsSolverTsunami propagationSettore ICAR/01 - IdraulicaThermal hydraulicsWetting/dryingWaves and shallow waterBoundary layerNon-hydrostatic pressureDirichlet conditionFluid dynamicsRunge-Kutta methodOpenFOAMMagnetohydrodynamicsNavier–Stokes equationsGalerkin schemeGeologyManning equation
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ON THE BOUSSINESQ HIERARCHY

2002

A new sequence of nonlinear evolution systems satisfying the zero curvature property is constructed, by using the invariant singularity analysis. All these systems are completely integrable and a pseudo-potential (linearization) is explicitly determined for each of them. The second system of the sequence is the Broer-Kaup system, which, as is well known, corresponds to the higher order Boussinesq approximation in describing shallow water waves.

Waves and shallow waterIntegrable systemLinearizationSingularity analysisMathematical analysisBoussinesq approximation (water waves)CurvatureNonlinear evolutionMathematicsWaves and Stability in Continuous Media
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