Search results for "Continuity"

showing 10 items of 378 documents

Hölder stability for Serrin’s overdetermined problem

2015

In a bounded domain \(\varOmega \), we consider a positive solution of the problem \(\Delta u+f(u)=0\) in \(\varOmega \), \(u=0\) on \(\partial \varOmega \), where \(f:\mathbb {R}\rightarrow \mathbb {R}\) is a locally Lipschitz continuous function. Under sufficient conditions on \(\varOmega \) (for instance, if \(\varOmega \) is convex), we show that \(\partial \varOmega \) is contained in a spherical annulus of radii \(r_i 0\) and \(\tau \in (0,1]\). Here, \([u_\nu ]_{\partial \varOmega }\) is the Lipschitz seminorm on \(\partial \varOmega \) of the normal derivative of u. This result improves to Holder stability the logarithmic estimate obtained in Aftalion et al. (Adv Differ Equ 4:907–93…

Applied Mathematics010102 general mathematicsMathematical analysisRegular polygonSerrin’s problemFunction (mathematics)Directional derivativeLipschitz continuity01 natural sciencesDomain (mathematical analysis)010101 applied mathematicsOverdetermined systemCombinatoricsBounded functionOverdetermined problemHarnack’s inequalityStationary surface0101 mathematicsStabilityMethod of moving planeHarnack's inequalityMathematicsAnnali di Matematica Pura ed Applicata (1923 -)
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Isoperimetric inequality via Lipschitz regularity of Cheeger-harmonic functions

2014

Abstract Let ( X , d , μ ) be a complete, locally doubling metric measure space that supports a local weak L 2 -Poincare inequality. We show that optimal gradient estimates for Cheeger-harmonic functions imply local isoperimetric inequalities.

Applied MathematicsGeneral Mathematics010102 general mathematicsMathematical analysista111Poincaré inequalityIsoperimetric dimensionSpace (mathematics)Lipschitz continuity01 natural sciencesMeasure (mathematics)symbols.namesakeHarmonic function0103 physical sciencesMetric (mathematics)symbolsMathematics::Metric Geometry010307 mathematical physics0101 mathematicsIsoperimetric inequalityMathematicsJournal de Mathématiques Pures et Appliquées
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Singular integrals on regular curves in the Heisenberg group

2019

Let $\mathbb{H}$ be the first Heisenberg group, and let $k \in C^{\infty}(\mathbb{H} \, \setminus \, \{0\})$ be a kernel which is either odd or horizontally odd, and satisfies $$|\nabla_{\mathbb{H}}^{n}k(p)| \leq C_{n}\|p\|^{-1 - n}, \qquad p \in \mathbb{H} \, \setminus \, \{0\}, \, n \geq 0.$$ The simplest examples include certain Riesz-type kernels first considered by Chousionis and Mattila, and the horizontally odd kernel $k(p) = \nabla_{\mathbb{H}} \log \|p\|$. We prove that convolution with $k$, as above, yields an $L^{2}$-bounded operator on regular curves in $\mathbb{H}$. This extends a theorem of G. David to the Heisenberg group. As a corollary of our main result, we infer that all …

Applied MathematicsGeneral Mathematics42B20 (primary) 43A80 28A75 35R03 (secondary)Metric Geometry (math.MG)Singular integralLipschitz continuityuniform rectifiabilityHeisenberg groupFunctional Analysis (math.FA)ConvolutionBounded operatorMathematics - Functional AnalysisCombinatoricsMathematics - Metric GeometryMathematics - Classical Analysis and ODEsBounded functionClassical Analysis and ODEs (math.CA)FOS: MathematicsHeisenberg groupsingular integralsBoundary value problemKernel (category theory)MathematicsJournal de Mathématiques Pures et Appliquées
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Approximation and quasicontinuity of Besov and Triebel–Lizorkin functions

2016

We show that, for $0<s<1$, $0<p<\infty$, $0<q<\infty$, Haj\l asz-Besov and Haj\l asz-Triebel-Lizorkin functions can be approximated in the norm by discrete median convolutions. This allows us to show that, for these functions, the limit of medians, \[ \lim_{r\to 0}m_u^\gamma(B(x,r))=u^*(x), \] exists quasieverywhere and defines a quasicontinuous representative of $u$. The above limit exists quasieverywhere also for Haj\l asz functions $u\in M^{s,p}$, $0<s\le 1$, $0<p<\infty$, but approximation of $u$ in $M^{s,p}$ by discrete (median) convolutions is not in general possible.

Applied MathematicsGeneral Mathematicsmedian010102 general mathematicsMathematical analysista111QuasicontinuityMedianMetric measure space010103 numerical & computational mathematicsTriebel–Lizorkin spaceTriebel–Lizorkin space01 natural sciencesFractional Sobolev spaceCombinatoricsmetric measure spaceBesov spacequasicontinuityLimit (mathematics)0101 mathematicsBesov spacefractional Sobolev spaceMathematicsTRANSACTIONS OF THE AMERICAN MATHEMATICAL SOCIETY
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Monotonicity-based inversion of the fractional Schr\"odinger equation II. General potentials and stability

2019

In this work, we use monotonicity-based methods for the fractional Schr\"odinger equation with general potentials $q\in L^\infty(\Omega)$ in a Lipschitz bounded open set $\Omega\subset \mathbb R^n$ in any dimension $n\in \mathbb N$. We demonstrate that if-and-only-if monotonicity relations between potentials and the Dirichlet-to-Neumann map hold up to a finite dimensional subspace. Based on these if-and-only-if monotonicity relations, we derive a constructive global uniqueness results for the fractional Calder\'on problem and its linearized version. We also derive a reconstruction method for unknown obstacles in a given domain that only requires the background solution of the fractional Sch…

Applied MathematicsMathematical analysisOpen setMonotonic functionLipschitz continuity01 natural sciencesInversion (discrete mathematics)Stability (probability)OmegaSchrödinger equation010101 applied mathematicsComputational Mathematicssymbols.namesakeMathematics - Analysis of PDEs35R30Bounded functionsymbols0101 mathematicsAnalysisMathematics
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Long-term persistence, invariant time scales and on-off intermittency of fog events

2021

Abstract In this work we study different characteristics of fog long-term persistence, in events with different physical formation mechanisms. Specifically, we focus on the characterization of fog long-term persistence from observational data, by means of a Detrended Fluctuation Analysis (DFA) of its associated low-visibility time series. We analyze fog events with radiation and orographic underlying physical formation mechanisms, and identify a two-range pattern of long-term persistence. Our analysis leads to the emergence of a characteristic time, τ∗, at the crossover point between different scaling exponents in the DFA, independent of the time scale at which the fog event is studied. We …

Atmospheric SciencelawIntermittencyCrossoverDetrended fluctuation analysisEnvironmental scienceStatistical physicsInvariant (physics)Persistence (discontinuity)ScalingEvent (probability theory)Orographic liftlaw.inventionAtmospheric Research
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Autocorrelation Metrics to Estimate Soil Moisture Persistence From Satellite Time Series: Application to Semiarid Regions

2021

Satellite-derived soil moisture (SM) products have become an important information source for the study of land surface processes in hydrology and land monitoring. Characterizing and estimating soil memory and persistence from satellite observations is of paramount relevance, and has deep implications in ecology, water management, and climate modeling. In this work, we address the problem of SM persistence estimation from microwave sensors using several autocorrelation metrics that, unlike traditional approaches, build on accurate estimates of the autocorrelation function from nonuniformly sampled time series. We show how the choice of the autocorrelation estimator can have a dramatic impac…

Autocorrelation0211 other engineering and technologiesEstimator02 engineering and technology15. Life on landScatterometer6. Clean waterPhysics::GeophysicsAdvanced Microwave Scanning Radiometer-2 (AMSR2) Advanced Scatterometer (ASCAT) autocorrelation e-folding time Least Absolute Shrinkage and Selection Operator (LASSO) Lomb-Scargle periodogram microwave sensors persistence soil moisture Soil Moisture and Ocean Salinity (SMOS) spatial-temporal13. Climate actionConsistency (statistics)General Earth and Planetary SciencesEnvironmental scienceClimate modelSatelliteElectrical and Electronic EngineeringTransectPersistence (discontinuity)021101 geological & geomatics engineeringRemote sensingIEEE Transactions on Geoscience and Remote Sensing
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Representable and Continuous Functionals on Banach Quasi *-Algebras

2017

In the study of locally convex quasi *-algebras an important role is played by representable linear functionals; i.e., functionals which allow a GNS-construction. This paper is mainly devoted to the study of the continuity of representable functionals in Banach and Hilbert quasi *-algebras. Some other concepts related to representable functionals (full-representability, *-semisimplicity, etc) are revisited in these special cases. In particular, in the case of Hilbert quasi *-algebras, which are shown to be fully representable, the existence of a 1-1 correspondence between positive, bounded elements (defined in an appropriate way) and continuous representable functionals is proved.

Banach quasi *-algebraGeneral MathematicsHilbert quasi01 natural sciencesRepresentable functionalsAutomatic continuity of representable functional0103 physical sciencesFOS: MathematicsMathematics (all)Banach quasi0101 mathematicsOperator Algebras (math.OA)MathematicsDiscrete mathematics010102 general mathematicsMathematics - Operator AlgebrasRegular polygonAutomatic continuity of representable functionalsFunctional Analysis (math.FA)Mathematics - Functional AnalysisAutomatic continuity of representable functionals; Banach quasi; Hilbert quasi; Representable functionals; MathematicsRepresentable functionalBounded functionHilbert quasi *-algebra010307 mathematical physicsMathematicsMediterranean Journal of Mathematics
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Influence of a thin horizontal weak layer on the mechanical behaviour of shallow foundations resting on sand

2021

The presence of minor details of the ground, including soil or rock masses, occurs more frequently than what is normally believed. Thin weak layers, shear bands, and slickensided surfaces can substantially affect the behaviour of foundations, as well as that of other geostructures. In fact, they can affect the failure mechanisms, the ultimate bearing capacity of footings, and the safety factor of the geotechnical system. In this research, numerically conducted through Finite Element Code Plaxis 2D, the influence of a horizontal thin weak layer on the mechanical behaviour of shallow footings was evaluated. The obtained results prove that the weak layer strongly influences both the failure me…

Bearing capacityQE1-996.5FEMSafety factorSettore ICAR/07 - GeotecnicaFoundation (engineering)GeologyWeak layerFinite element methodShear (sheet metal)Shallow foundationFailure mechanismsGeneral Earth and Planetary SciencesGeotechnical engineeringBearing capacityLayer (electronics)Shear strength (discontinuity)GeologyStrip footing
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Experimental observations of upstream overdeepening

2005

The issue of morphodynamic influence in meandering streams is investigated through a series of laboratory experiments on curved and straight flumes. Both qualitative and quantitative observations confirm the suitability of the recent theoretical developments (Zolezzi & Seminara 2001) that indicate the occurrence of two distinct regimes of morphodynamic influence, depending on the value of the width ratio of the channel β. The threshold value βR separating the upstream from the downstream influence regimes coincides with the resonant value discovered by Blondeaux & Seminara (1985). Indeed it is observed that upstream influence may occur only in relatively wide channels, while narrower stream…

BedformMechanics of MaterialsMechanical EngineeringOverdeepeningThe issue of morphodynamic influence in meandering streams is investigated through a series of laboratory experiments on curved and straight flumes. Both qualitative and quantitative observations confirm the suitability of the recent theoretical developments (Zolezzi & Seminara 2001) that indicate the occurrence of two distinct regimes of morphodynamic influence depending on the value of the width ratio of the channel β. The threshold value βR separating the upstream from the downstream influence regimes coincides with the resonant value discovered by Blondeaux & Seminara (1985). Indeed it is observed that upstream influence may occur only in relatively wide channels while narrower streams are dominated by downstream influence. A series of experiments has been carried out in order to check the above theoretical predictions and show for the first time evidence of the occurrence of upstream overdeepening. Two different sets of experiments have been designed where a discontinuity in channel geometry was present such that the channel morphodynamics was influenced in the upstream direction under super-resonant conditions (β >βR) and in the downstream direction under sub-resonant conditions (β <βR). Experimental results give qualitative and quantitative support to the theoretical predictions and allow us to clarify the limits of the linear analysis.MechanicsLinear analysisCondensed Matter PhysicsWidth ratioGeology
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