Search results for "Convection"

showing 10 items of 332 documents

Acoustic and optical variations during rapid downward motion episodes in the deep north-western Mediterranean Sea

2011

An Acoustic Doppler Current Profiler (ADCP) was moored at the deep-sea site of the ANTARES neutrino telescope near Toulon, France, thus providing a unique opportunity to compare high-resolution acoustic and optical observations between 70 and 170 m above the sea bed at 2475 m. The ADCP measured downward vertical currents of magnitudes up to 0.03 m s-1 in late winter and early spring 2006. In the same period, observations were made of enhanced levels of acoustic reflection, interpreted as suspended particles including zooplankton, by a factor of about 10 and of horizontal currents reaching 0.35 m s-1. These observations coincided with high light levels detected by the telescope, interpreted …

Optical telescopesDense water formation010504 meteorology & atmospheric sciencesDense watersBoundary currentWave reflectionOptical photo-multiplier observationsSuspended loadWATER FORMATIONOceanography01 natural scienceslaw.inventionPhysics - GeophysicsObservational methodMediterranean sea86-02lawDeep MediteraneanSeabedPhosphorescenceDeep seaCurrent (stream)VARIABILITYOptical methodOceanographyAcoustic variables measurementNorthern boundary currentantares neutrino telescope; deep mediteranean; northern boundary current; acoustic adcp observations; episodic downward current; dense water formation; bioluminescence; optical photo-multiplier observationsFísica nuclearAcoustic Doppler Current ProfilerBioluminescenceAstrophysics - Instrumentation and Methods for AstrophysicsANTARES neutrino telescopeGeology[PHYS.ASTR.IM]Physics [physics]/Astrophysics [astro-ph]/Instrumentation and Methods for Astrophysic [astro-ph.IM]Acoustic ADCP observationsCIRCULATIONFOS: Physical sciencesAquatic ScienceLIGURIAN SEAZooplanktonZooplanktonTelescopeAcoustic Doppler current profilerOCEANOPTICAL PHOTO-MULTIPLIERMediterranean Sea14. Life underwaterInstrumentation and Methods for Astrophysics (astro-ph.IM)0105 earth and related environmental sciencesLight reflectionANTARESAcoustic wave010505 oceanographyAdvectionDense waterElementary particlesZOOPLANKTON BIOMASSDoppler effectMARINE RESEARCHESGeophysics (physics.geo-ph)Boundary current[SDU.ASTR.IM]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Instrumentation and Methods for Astrophysic [astro-ph.IM]Boundary currentsCONVECTION13. Climate actionFISICA APLICADAAdvectionEpisodic downward currentMediterranean Sea (Northwest)SYSTEMTelescopes
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Three-Dimensional Flow and Temperature Distribution in Rayleigh-Bènard Convection Using Thermochromic Liquid Crystals and Digital Image Processing

2000

PIVNatural ConvectionThermochromic Liquid CrystalDigital Image ProcessingThermographyRectangular EnclosureRayleigh-Bénard ConvectionSettore ING-IND/19 - Impianti Nucleari
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Improved Tomographic Particle Image Velocimetry and Thermography in Rayleigh-Bènard Convection

2001

PIVNatural ConvectionThermochromic Liquid CrystalThermographyRectangular EnclosureRayleigh-Bénard ConvectionSettore ING-IND/19 - Impianti Nucleari
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Parallel Schwarz methods for convection-dominated semilinear diffusion problems

2002

AbstractParallel two-level Schwarz methods are proposed for the numerical solution of convection-diffusion problems, with the emphasis on convection-dominated problems. Two variants of the methodology are investigated. They differ from each other by the type of boundary conditions (Dirichlet- or Neumann-type) posed on a part of the second-level subdomain interfaces. Convergence properties of the two-level Schwarz methods are experimentally compared with those of a variant of the standard multi-domain Schwarz alternating method. Numerical experiments performed on a distributed memory multiprocessor computer illustrate parallel efficiency of the methods.

Parallel computingApplied MathematicsNumerical analysisMathematical analysisParallel algorithmDomain decomposition methodsSingularly perturbed semilinear convection–diffusion problemMulti-level Schwarz methodsComputational MathematicsAdditive Schwarz methodDistributed memoryBoundary value problemSchwarz alternating methodConvection–diffusion equationMathematicsJournal of Computational and Applied Mathematics
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Existence and uniqueness for the Prandtl equations

2001

International audience; Under the hypothesis of analyticity of the data with respect to the tangential variable we prove the existence and uniqueness of the mild solution of Prandtl boundary layer equation. This can be considered an improvement of the results of [8] as we do not require analyticity with respect to the normal variable. (C) 2001 Academie des sciences/Editions scientifiques et medicales Elsevier SAS.

Partial differential equation010102 general mathematicsPrandtl numberMathematical analysisGeneral Medicine01 natural sciencesEuler equations010101 applied mathematicssymbols.namesakeBoundary layer[MATH.MATH-MP]Mathematics [math]/Mathematical Physics [math-ph]symbolsUniqueness0101 mathematicsConvection–diffusion equationNavier–Stokes equationsVariable (mathematics)Mathematics
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Melt evolution beneath a rifted craton edge: 40Ar/39Ar geochronology and Sr-Nd-Hf-Pb isotope systematics of primitive alkaline basalts and lamprophyr…

2016

A new high-precision Ar-40/Ar-39 anorthoclase feldspar age of 176.7 +/- 0.5 Ma (2-sigma) reveals that small-volume alkaline basaltic magmatism occurred at the rifted SW margin of the Baltic Shield in Scania (southern Sweden), at a time of global plate reorganization associated with the inception of Pangea supercontinent break-up. Our combined elemental and Sr-Nd-Hf-Pb isotope dataset for representative basanite and nephelinite samples (>8 wt.% MgO) from 16 subvolcanic necks of the 30 by 40 km large Jurassic volcanic field suggests magma derivation from a moderately depleted mantle source (Sr-87/(86)Sri = 0.7034-0.7048; epsilon Nd-i = +4.4 to +5.2; epsilon Hf-i = +4.7 to +8.1; Pb-206/(204)Pb…

PeridotiteBasaltIncompatible elementgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistryPartial melting010502 geochemistry & geophysics01 natural sciencesMantle (geology)CratonMantle convectionGeochemistry and PetrologyBaltic ShieldGeology0105 earth and related environmental sciences
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Traces of ancient mafic layers in the Tethys oceanic mantle

2014

Abstract Oceanic basalts are formed by melting of a chemically and isotopically heterogeneous mantle source. The oceanic mantle probably resembles a marble cake containing layers of mafic rock – perhaps recycled ocean crust – stored in the mantle for >1 billion years. Many questions about the nature and distribution of these mantle heterogeneities remain. Here we show that lithological and isotopic traces of ancient mafic layers can still be seen in mantle rocks that have melted to form oceanic crust at a spreading centre in the Tethys Ocean. We have found centimetre-scale heterogeneity in initial osmium isotope ratios in mantle rocks from the Pindos Ophiolite. Deformed pyroxenite layers ha…

PeridotiteBasaltMantle wedgeGeochemistryOphioliteMantle (geology)GeophysicsMantle convectionSpace and Planetary ScienceGeochemistry and PetrologyOceanic crustTransition zoneEarth and Planetary Sciences (miscellaneous)GeologyEarth and Planetary Science Letters
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Effect of low mass dark matter particles on the Sun

2010

We study the effect of dark matter (DM) particles in the Sun, focusing in particular on the possible reduction of the solar neutrinos flux due to the energy carried away by DM particles from the innermost regions of the Sun, and to the consequent reduction of the temperature of the solar core. We find that in the very low-mass range between 4 and 10 GeV, recently advocated to explain the findings of the DAMA and CoGent experiments, the effects on neutrino fluxes are detectable only for DM models with very small, or vanishing, self-annihilation cross section, such as the so-called asymmetric DM models, and we study the combination of DM masses and Spin Dependent cross sections which can be e…

PhysicsAstrophysics and AstronomyNuclear and High Energy PhysicsCosmology and Nongalactic Astrophysics (astro-ph.CO)Solar energetic particles010308 nuclear & particles physics530 PhysicsSolar neutrinoDark matterFOS: Physical sciencesAstrophysics01 natural sciencesMassless particleHigh Energy Physics - PhenomenologyHigh Energy Physics - Phenomenology (hep-ph)Solar coreConvection zone10231 Institute for Computational Science0103 physical sciencesNeutrino3106 Nuclear and High Energy Physics3101 Physics and Astronomy (miscellaneous)010303 astronomy & astrophysicsLeptonAstrophysics - Cosmology and Nongalactic Astrophysics
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A large X-ray flare from the Herbig Ae star V892 Tau

2003

We report the XMM-Newton observation of a large X-ray flare from the Herbig Ae star V892 Tau. The apparent low mass companion of V892 Tau, V892 Tau NE, is unresolved by XMM-Newton. Nevertheless there is compelling evidence from combined XMM-Newton and Chandra data that the origin of the flare is the Herbig Ae star V892 Tau. During the flare the X-ray luminosity of V892 Tau increases by a factor of ~15, while the temperature of the plasma increases from kT ~ 1.5 keV to kT ~ 8 keV. From the scaling of the flare event, based on hydrodynamic modeling, we conclude that a 500 G magnetic field is needed in order to confine the plasma. Under the assumptions that a dynamo mechanism is required to ge…

PhysicsAstrophysics::High Energy Astrophysical PhenomenaAstrophysics (astro-ph)FOS: Physical sciencesAstronomy and AstrophysicsPlasmaAstrophysicsAstrophysics::Cosmology and Extragalactic AstrophysicsAstrophysicsMagnetic fieldLuminositylaw.inventiondisks protoplanetary disks outer diskStarsConvection zoneSpace and Planetary SciencelawAstrophysics::Solar and Stellar AstrophysicsAstrophysics::Earth and Planetary AstrophysicsLow MassAstrophysics::Galaxy AstrophysicsFlareDynamo
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Refrigeration of an Array of Cylindrical Nanosystems by Flowing Superfluid Helium

2016

We consider the refrigeration of an array of heat-dissipating cylindrical nanosystems as a simplified model of computer refrigeration. We explore the use of He II as cooling fluid, taking into account forced convection and heat conduction. The main conceptual and practical difficulties arise in the calculation of the effective thermal conductivity. Since He II does not follow Fourier’s law, the effective geometry-dependent conductivity must be extracted from a more general equation for heat transfer. Furthermore, we impose the restrictions that the maximum temperature along the array should be less than (Formula presented.) transition temperature and that quantum turbulence is avoided, in o…

PhysicsCondensed matter physicsQuantum turbulenceRefrigerationConductivityCondensed Matter PhysicsThermal conduction01 natural sciencesNanorefrigerationAtomic and Molecular Physics and Optics010305 fluids & plasmasForced convectionThermal conductivityThermal conductivity0103 physical sciencesHeat transferGeneral Materials ScienceSuperfluid helium010306 general physicsSettore MAT/07 - Fisica MatematicaSuperfluid helium-4Journal of Low Temperature Physics
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