Search results for "solution"

showing 10 items of 5638 documents

Time-harmonic solution for acousto-elastic interaction with controllability and spectral elements

2010

The classical way of solving the time-harmonic linear acousto-elastic wave problem is to discretize the equations with finite elements or finite differences. This approach leads to large-scale indefinite complex-valued linear systems. For these kinds of systems, it is difficult to construct efficient iterative solution methods. That is why we use an alternative approach and solve the time-harmonic problem by controlling the solution of the corresponding time dependent wave equation. In this paper, we use an unsymmetric formulation, where fluid-structure interaction is modeled as a coupling between pressure and displacement. The coupled problem is discretized in space domain with spectral el…

ControllabilityDiscretizationSpectral element methodfluid-structure interactionspectral element methodacoustic wavescoupled problemTime-harmonic solutioncontrollabilityConjugate gradient methodFluid-structure interactionTime domainCoupled problemMathematicsElastic wavesSpectral element methodelastic wavestime-harmonic solutionApplied MathematicsMathematical analysisLinear systemFinite differenceFinite element methodControllabilityComputational MathematicsAcoustic wavesConjugate gradient algorithmconjugate gradient algorithmJournal of Computational and Applied Mathematics
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Singular Double Phase Problems with Convection

2020

We consider a nonlinear Dirichlet problem driven by the sum of a $p$ -Laplacian and of a $q$ -Laplacian (double phase equation). In the reaction we have the combined effects of a singular term and of a gradient dependent term (convection) which is locally defined. Using a mixture of variational and topological methods, together with suitable truncation and comparison techniques, we prove the existence of a positive smooth solution.

ConvectionDirichlet problemPartial differential equationTruncationApplied Mathematics010102 general mathematicsMathematical analysisSingular termFixed pointMathematics::Spectral Theory01 natural sciencesTerm (time)Positive solution010101 applied mathematicsNonlinear system(p q)-LaplacianSettore MAT/05 - Analisi MatematicaNonlinear maximum principle0101 mathematicsLaplace operatorNonlinear regularityMathematicsActa Applicandae Mathematicae
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A PCA-based clustering algorithm for the identification of stratiform and convective precipitation at the event scale: an application to the sub-hour…

2021

AbstractUnderstanding the structure of precipitation and its separation into stratiform and convective components is still today one of the important and interesting challenges for the scientific community. Despite this interest and the advances made in this field, the classification of rainfall into convective and stratiform components is still today not trivial. This study applies a novel criterion based on a clustering approach to analyze a high temporal resolution precipitation dataset collected for the period 2002–2018 over the Sicily (Italy). Starting from the rainfall events obtained from this dataset, the developed methodology makes it possible to classify the rainfall events into f…

ConvectionEnvironmental Engineering010504 meteorology & atmospheric sciencesFunctional data analysis01 natural sciencesExtreme rainfall Convective and stratiform precipitation Functional data analysis PCA-based clustering analysis010104 statistics & probabilityIdentification (information)HyetographClimatologyTemporal resolutionEnvironmental ChemistryPrecipitation0101 mathematicsSafety Risk Reliability and QualityCluster analysisGeology0105 earth and related environmental sciencesGeneral Environmental ScienceWater Science and TechnologyConvective precipitation
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Positive solutions for nonlinear Robin problems with convection

2019

We consider a nonlinear Robin problem driven by the p-Laplacian and with a convection term f(z,x,y). Without imposing any global growth condition on f(z,·,·) and using topological methods (the Leray-Schauder alternative principle), we show the existence of a positive smooth solution.

ConvectionGeneral Mathematicsnonlinear maximum principlep-LaplacianGeneral Engineering(minimal) positive solutionNonlinear systemEngineering (all)p-LaplacianApplied mathematicsnonlinear regularityMathematics (all)convection termLeray-Schauder alternative principleMathematics
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Variable exponent p(x)-Kirchhoff type problem with convection

2022

Abstract We study a nonlinear p ( x ) -Kirchhoff type problem with Dirichlet boundary condition, in the case of a reaction term depending also on the gradient (convection). Using a topological approach based on the Galerkin method, we discuss the existence of two notions of solutions: strong generalized solution and weak solution. Strengthening the bound on the Kirchhoff type term (positivity condition), we establish existence of weak solution, this time using the theory of operators of monotone type.

ConvectionKirchhoff type termApplied MathematicsWeak solutionMathematical analysisWeak solutionGeneralized solutionType (model theory)ConvectionTerm (time)Pseudomonotone operatorNonlinear systemsymbols.namesakeMonotone polygonGalerkin basisSettore MAT/05 - Analisi MatematicaDirichlet boundary conditionsymbolsGalerkin methodAnalysisMathematics
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Fronts propagating with signal dependent speed in limited diffusion and related Hamilton-Jacobi formulations

2021

We consider a class of limited diffusion equations and explore the formation of diffusion fronts as the result of a combination of diffusive and hyperbolic transport. We analyze a new class of Hamilton-Jacobi equations arising from the convective part of general Fokker-Planck equations ruled by a non-negative diffusion coefficient that depends on the unknown and on the gradient of the unknown. We explore the main features of the solution of the Hamilton-Jacobi equations that contain shocks and propose a suitable numerical scheme that approximates the solution in a consistent way with respect to the solution of the associated Fokker-Planck equation. We analyze three model problems covering d…

ConvectionNumerical AnalysisDarcy's lawNumerical approximationApplied MathematicsMathematical analysisFunction (mathematics)Hamilton–Jacobi equationComputational MathematicsLimited diffusion equationsPiecewiseHeat equationDiffusion (business)Constant (mathematics)Hamilton-Jacobi equationsViscosity solutions with shocksMathematics
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Magnetic field emergence in mesogranular-sized exploding granules observed with SUNRISE/IMaX data

2011

We report on magnetic field emergences covering significant areas of exploding granules. The balloon-borne mission SUNRISE provided high spatial and temporal resolution images of the solar photosphere. Continuum images, longitudinal and transverse magnetic field maps and Dopplergrams obtained by IMaX onboard SUNRISE are analyzed by Local Correlation Traking (LCT), divergence calculation and time slices, Stokes inversions and numerical simulations are also employed. We characterize two mesogranular-scale exploding granules where $\sim$ 10$^{18}$ Mx of magnetic flux emerges. The emergence of weak unipolar longitudinal fields ($\sim$100 G) start with a single visible magnetic polarity, occupyi…

ConvectionPhysicsAdvectionFOS: Physical sciencesAstronomy and AstrophysicsPlasmaAstrophysicsMagnetic fluxMagnetic fieldAstrophysics - Solar and Stellar AstrophysicsSpace and Planetary ScienceTemporal resolutionSunriseAstrophysics::Solar and Stellar AstrophysicsMagnetohydrodynamicsSolar and Stellar Astrophysics (astro-ph.SR)
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Multiple solutions with sign information for semilinear Neumann problems with convection

2019

We consider a semilinear Neumann problem with convection. We assume that the drift coefficient is indefinite. Using the theory of nonlinear operators of monotone type, together with truncation and comparison techniques and flow invariance arguments, we prove a multiplicity theorem producing three nontrivial smooth solutions (positive, negative and nodal).

ConvectionTruncationGeneral Mathematics010102 general mathematicsMathematical analysisMultiplicity (mathematics)Type (model theory)Convection01 natural sciencesIndefinite drift coefficientExtremal constant sign solution010101 applied mathematicsMonotone polygonFlow (mathematics)Settore MAT/05 - Analisi MatematicaConstant sign and nodal solutionNeumann boundary conditionFlow invariance0101 mathematicsSign (mathematics)MathematicsRevista Matemática Complutense
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Onset of convection in a porous rectangular channel with external heat transfer to upper and lower fluid environments

2012

Published version of an article in the journal: Transport in Porous Media. Also available from the publisher at: http://dx.doi.org/10.1007/s11242-012-0018-9 The conditions for the onset of convection in a horizontal rectangular channel filled with a fluid saturated porous medium are studied. The vertical sidewalls are assumed to be impermeable and adiabatic. The horizontal upper and lower boundary walls are considered as impermeable and subject to external heat transfer, modelled through a third-kind boundary condition on the temperature field. The external fluid environments above and below the channel, kept at different temperatures, provide the heating-from-below mechanism which may lead…

ConvectionVDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413Materials scienceDarcy's lawBiot numberGeneral Chemical EngineeringThermodynamicsMechanicsCatalysisPhysics::Fluid Dynamicsanalytical solutionDarcy’s lawHeat transferBoundary value problemVDP::Technology: 500::Materials science and engineering: 520Porous mediumAdiabatic processrectangular porous channelDarcy–Bénard problemLongitudinal wavelinear stabilitythird-kind temperature conditions
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Quasilinear Dirichlet Problems with Degenerated p-Laplacian and Convection Term

2021

The paper develops a sub-supersolution approach for quasilinear elliptic equations driven by degenerated p-Laplacian and containing a convection term. The presence of the degenerated operator forces a substantial change to the functional setting of previous works. The existence and location of solutions through a sub-supersolution is established. The abstract result is applied to find nontrivial, nonnegative and bounded solutions.

Convectionsub-supersolutionGeneral MathematicsOperator (physics)quasilinear elliptic problemlcsh:MathematicsMathematical analysisMathematics::Analysis of PDEsnonnegative solutionlcsh:QA1-939Dirichlet distributionTerm (time)symbols.namesakedegenereted p-LaplacianSettore MAT/05 - Analisi MatematicaBounded functionComputer Science (miscellaneous)p-Laplaciansymbolsconvection termEngineering (miscellaneous)MathematicsMathematics
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