Search results for "Geodetic datum"

showing 10 items of 21 documents

Towards Understanding the Interconnection between Celestial Pole Motion and Earth’s Magnetic Field Using Space Geodetic Techniques

2021

The understanding of forced temporal variations in celestial pole motion (CPM) could bring us significantly closer to meeting the accuracy goals pursued by the Global Geodetic Observing System (GGOS) of the International Association of Geodesy (IAG), i.e., 1 mm accuracy and 0.1 mm/year stability on global scales in terms of the Earth orientation parameters. Besides astronomical forcing, CPM excitation depends on the processes in the fluid core and the core–mantle boundary. The same processes are responsible for the variations in the geomagnetic field (GMF). Several investigations were conducted during the last decade to find a possible interconnection of GMF changes with the length of day (…

010504 meteorology & atmospheric sciencesMotion (geometry)TP1-1185010502 geochemistry & geophysicsSpace (mathematics)01 natural sciencesBiochemistryArticleAnalytical ChemistryPhysics::Geophysicscelestial pole offsetCelestial polegeomagnetic fieldCelestial pole offsetVery-long-baseline interferometryElectrical and Electronic EngineeringInstrumentation0105 earth and related environmental sciencesPhysicsInterconnectionChemical technologyEuropean researchGeodetic datumMatemática AplicadaGeodesyAtomic and Molecular Physics and OpticsEarth's magnetic field13. Climate actionPhysics::Space Physicsddc:620VLBIGeomagnetic fieldSensors
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Software development and its description for Geoid determination based on Spherical-Cap-Harmonics Modelling using digital-zenith camera and gravimetr…

2017

Over several years the Institute of Geodesy and Geoinformatics (GGI) was engaged in the design and development of a digital zenith camera. At the moment the camera developments are finished and tests by field measurements are done. In order to check these data and to use them for geoid model determination DFHRS (Digital Finite element Height reference surface (HRS)) v4.3. software is used. It is based on parametric modelling of the HRS as a continous polynomial surface. The HRS, providing the local Geoid height N, is a necessary geodetic infrastructure for a GNSS-based determination of physcial heights H from ellipsoidal GNSS heights h, by H=h-N. The research and this publication is dealing…

010504 meteorology & atmospheric sciencesbusiness.industryComputationSoftware developmentGeodetic datum010502 geochemistry & geophysicsGeodesy01 natural sciencesSoftwareGeographyGNSS applicationsGeoidReference surfaceZenith camerabusiness0105 earth and related environmental sciencesRemote sensingIOP Conference Series: Materials Science and Engineering
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Geodetic and geological evidence of active tectonics in south-western Sicily (Italy)

2014

Abstract Integrated geological, geodetic and marine geophysical data provide evidence of active deformation in south-western Sicily, in an area spatially coincident with the macroseismic zone of the destructive 1968 Belice earthquake sequence. Even though the sequence represents the strongest seismic event recorded in Western Sicily in historical times, focal solutions provided by different authors are inconclusive on possible faulting mechanism, which ranges from thrusting to transpression, and the seismogenic source is still undefined. Interferometric (DInSAR) observations reveal a differential ground motion on a SW–NE alignment between Campobello di Mazara and Castelvetrano (CCA), locate…

Active tectonicsPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleGeodetic datumSicilian fold and thrust belt; Geodesy; Active tectonicsaActive faultTranspressionTectonicsSequence (geology)GeophysicsSeismic hazardThrust faultActive tectonicsaGeologySeismologySicilian fold and thrust beltGeodesyEarth-Surface ProcessesSicilian fold and thrust belt; Geodesy; Active tectonics
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Existence results and asymptotic behavior for nonlocal abstract Cauchy problems

2008

AbstractThe purpose of this paper is to study the existence and asymptotic behavior of solutions for Cauchy problems with nonlocal initial datum generated by accretive operators in Banach spaces.

Cauchy problemPure mathematicsm-Accretive operatorsNonlocal Cauchy problemsApplied MathematicsMathematical analysisBanach spaceMathematics::Analysis of PDEsGeodetic datumCauchy distributionIntegral solutionsAsymptotic behaviorAnalysisMathematicsJournal of Mathematical Analysis and Applications
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Some qualitative properties for the total variation flow

2002

We prove the existence of a finite extinction time for the solutions of the Dirichlet problem for the total variation flow. For the Neumann problem, we prove that the solutions reach the average of its initial datum in finite time. The asymptotic profile of the solutions of the Dirichlet problem is also studied. It is shown that the profiles are nonzero solutions of an eigenvalue-type problem that seems to be unexplored in the previous literature. The propagation of the support is analyzed in the radial case showing a behaviour entirely different to the case of the problem associated with the p-Laplacian operator. Finally, the study of the radially symmetric case allows us to point out othe…

Dirichlet problemAsymptotic behaviourMathematical analysisGeodetic datumElliptic boundary value problemOperator (computer programming)Dirichlet eigenvaluePropagation of the supportFlow (mathematics)Neumann boundary conditionNonlinear parabolic equationsPoint (geometry)Total variation flowEigenvalue type problemAnalysisMathematics
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Elliptic equations having a singular quadratic gradient term and a changing sign datum

2012

In this paper we study a singular elliptic problem whose model is \begin{eqnarray*} - \Delta u= \frac{|\nabla u|^2}{|u|^\theta}+f(x), in \Omega\\ u = 0, on \partial \Omega; \end{eqnarray*} where $\theta\in (0,1)$ and $f \in L^m (\Omega)$, with $m\geq \frac{N}{2}$. We do not assume any sign condition on the lower order term, nor assume the datum $f$ has a constant sign. We carefully define the meaning of solution to this problem giving sense to the gradient term where $u=0$, and prove the existence of such a solution. We also discuss related questions as the existence of solutions when the datum $f$ is less regular or the boundedness of the solutions when the datum $f \in L^m (\Omega)$ with …

Dirichlet problemPure mathematicsApplied MathematicsMathematical analysissingularity at zeroMathematics::Analysis of PDEsGeodetic datumTerm (logic)Omegadata with non-constant signdata with non-constant sign; dirichlet problem; singularity at zero; gradient termQuadratic equationgradient termNabla symboldirichlet problemConstant (mathematics)AnalysisMathematicsSign (mathematics)Communications on Pure and Applied Analysis
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Symmetrization for singular semilinear elliptic equations

2012

In this paper, we prove some comparison results for the solution to a Dirichlet problem associated with a singular elliptic equation and we study how the summability of such a solution varies depending on the summability of the datum f. © 2012 Fondazione Annali di Matematica Pura ed Applicata and Springer-Verlag.

Dirichlet problemSharp a priori estimatesSemilinear elliptic equationsMathematics::Operator AlgebrasApplied MathematicsMathematical analysisMathematics::Classical Analysis and ODEsMathematics::Analysis of PDEsComparison resultsSymmetrizationGeodetic datumElliptic curveSettore MAT/05 - Analisi MatematicaMathematics::K-Theory and HomologySymmetrizationMathematics
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Existence and comparison results for a singular semilinear elliptic equation with a lower order term

2014

This paper deals with the homogeneous Dirichlet problem for a singular semilinear elliptic equation with a first order term. When the datum is bounded we prove an existence result and we show that any solution can be compared with the solution to a suitable symmetrized problem.

Dirichlet problemSharp a priori estimatesSingular elliptic problems with gradient termApplied MathematicsGeneral MathematicsNumerical analysisMathematical analysisMathematics::Analysis of PDEsGeodetic datumSymmetrizationTerm (time)Elliptic curveSingular solutionSettore MAT/05 - Analisi MatematicaBounded functionSymmetrizationMathematics
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Large solutions for nonlinear parabolic equations without absorption terms

2012

In this paper we give a suitable notion of entropy solution of parabolic $p-$laplacian type equations with $1\leq p<2$ which blows up at the boundary of the domain. We prove existence and uniqueness of this type of solutions when the initial data is locally integrable (for $1<p<2$) or integrable (for $p=1$; i.e the Total Variation Flow case).

Entropy solutionsIntegrable systemMathematical analysisp-LaplacianMathematics::Analysis of PDEsGeodetic datumNonlinear parabolic equationsMathematics - Analysis of PDEsentropy solutions; large solutions; p-laplacian; total variation flowp-LaplacianFOS: MathematicsLarge solutionsUniquenessTotal variation flowEntropy (arrow of time)AnalysisMathematicsAnalysis of PDEs (math.AP)Journal of Functional Analysis
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On the relativistic heat equation in one space dimension

2012

We study the relativistic heat equation in one space dimension. We prove a local regularity result when the initial datum is locally Lipschitz in its support. We propose a numerical scheme that captures the known features of the solutions and allows for analysing further properties of their qualitative behaviour. J.A.C. acknowledges partial support by MINECO project, reference MTM2011-27739-C04-02, by GRC 2009 SGR 345 by the Generalitat de Catalunya, and by the Engineering and Physical Sciences Research Council grant number EP/K008404/1. J.A.C. also acknowledges support from the Royal Society through a Wolfson Research Merit Award. V.C. acknowledges partial support by MINECO project, refere…

General Mathematics010102 general mathematicsMathematical analysisSpace dimensionGeodetic datumLipschitz continuity01 natural sciences010101 applied mathematicsMathematics - Analysis of PDEsScheme (mathematics)FOS: MathematicsHeat equation0101 mathematicsMathematicsAnalysis of PDEs (math.AP)
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