Search results for "complex"

showing 10 items of 5889 documents

"Table 31" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged and neutral particles.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 4JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 27" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 4JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 28" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 5JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 32" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged and neutral particles.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 5JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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On vibrating thin membranes with mass concentrated near the boundary: an asymptotic analysis

2018

We consider the spectral problem \begin{equation*} \left\{\begin{array}{ll} -\Delta u_{\varepsilon}=\lambda(\varepsilon)\rho_{\varepsilon}u_{\varepsilon} & {\rm in}\ \Omega\\ \frac{\partial u_{\varepsilon}}{\partial\nu}=0 & {\rm on}\ \partial\Omega \end{array}\right. \end{equation*} in a smooth bounded domain $\Omega$ of $\mathbb R^2$. The factor $\rho_{\varepsilon}$ which appears in the first equation plays the role of a mass density and it is equal to a constant of order $\varepsilon^{-1}$ in an $\varepsilon$-neighborhood of the boundary and to a constant of order $\varepsilon$ in the rest of $\Omega$. We study the asymptotic behavior of the eigenvalues $\lambda(\varepsilon)$ and the eige…

Asymptotic analysisAsymptotic analysisBoundary (topology)Spectral analysis01 natural sciencesMathematics - Analysis of PDEsFOS: MathematicsBoundary value problem0101 mathematicsSteklov boundary conditionsMathematical physicsMathematicsApplied Mathematics010102 general mathematicsMathematical analysisZero (complex analysis)Order (ring theory)Asymptotic analysis; Eigenvalues; Mass concentration; Spectral analysis; Steklov boundary conditions; Analysis; Computational Mathematics; Applied MathematicsEigenvaluesEigenfunction010101 applied mathematicsComputational MathematicsBounded functionDomain (ring theory)Mass concentrationAnalysisAnalysis of PDEs (math.AP)
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Multiplicity results for asymptotically linear equations, using the rotation number approach

2007

By using a topological approach and the relation between rotation numbers and weighted eigenvalues, we give some multiplicity results for the boundary value problem u′′ + f(t, u) = 0, u(0) = u(T) = 0, under suitable assumptions on f(t, x)/x at zero and infinity. Solutions are characterized by their nodal properties.

Asymptotically linearGeneral MathematicsMultiplicity resultsmedia_common.quotation_subjectMathematical analysisZero (complex analysis)InfinityBoundary value problem continuation theorem shooting without uniqueness rotation number Sturm–Liouville Theory weighted eigenvalue multiplicity resultBoundary value problemRotation (mathematics)Eigenvalues and eigenvectorsRotation numberMathematicsmedia_common
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Causative role of oxidative stress in a Drosophila model of Friedreich ataxia

2006

Friedreich ataxia (FA), the most common form of hereditary ataxia, is caused by a deficit in the mitochondrial protein frataxin. While several hypotheses have been suggested, frataxin function is not well understood. Oxidative stress has been suggested to play a role in the pathophysiology of FA, but this view has been recently questioned, and its link to frataxin is unclear. Here, we report the use of RNA interference (RNAi) to suppress the Drosophila frataxin gene (fh) expression. This model system parallels the situation in FA patients, namely a moderate systemic reduction of frataxin levels compatible with normal embryonic development. Under these conditions, fh-RNAi flies showed a shor…

AtaxiaBlotting WesternLongevityGene ExpressionCHO Cellsmedicine.disease_causeBiochemistryAconitaseMitochondrial ProteinsCricetulusRNA interferenceCricetinaeIron-Binding ProteinsGeneticsmedicineAnimalsDrosophila ProteinsRNA MessengerMolecular BiologyGeneAconitate HydrataseHyperoxiaGeneticsElectron Transport Complex IbiologyReverse Transcriptase Polymerase Chain ReactionSuccinate dehydrogenasefungiImmunohistochemistryCell biologySuccinate DehydrogenaseOxidative StressDrosophila melanogasterFriedreich AtaxiaFrataxinbiology.proteinRNA Interferencemedicine.symptomOxidative stressBiotechnologyThe FASEB Journal
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2017

Abstract. Concurrent in situ analyses of interstitial aerosol and cloud droplet residues have been conducted at the Schmücke mountain site during the Hill Cap Cloud Thuringia campaign in central Germany in September and October 2010. Cloud droplets were sampled from warm clouds (temperatures between −3 and +16 °C) by a counterflow virtual impactor and the submicron-sized residues were analyzed by a compact time-of-flight aerosol mass spectrometer (C-ToF-AMS), while the interstitial aerosol composition was measured by an high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). During cloud-free periods, the submicron out-of-cloud aerosol was analyzed using both instruments, all…

Atmospheric Science010504 meteorology & atmospheric sciences010501 environmental sciencescomplex mixtures01 natural sciencesAerosolAmmoniachemistry.chemical_compoundchemistryNitrateNitric acidEnvironmental chemistryAmmoniumsense organsSulfateScavengingMass fraction0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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African volcanic emissions influencing atmospheric aerosols over the Amazon rain forest

2018

Long-range transport (LRT) plays an important role in the Amazon rain forest by bringing in different primary and secondary aerosol particles from distant sources. The atmospheric oxidation of dimethyl sulfide (DMS), emitted from marine plankton, is considered an important sulfate source over the Amazon rain forest, with a lesser contribution from terrestrial soil and vegetation sulfur emissions. Volcanic sulfur emissions from Africa could be a source of particulate sulfate to the Amazonian atmosphere upon transatlantic transport but no observations have been published. By using satellite observations, together with ground‑based and airborne aerosol particle observations, this paper provide…

Atmospheric Science010504 meteorology & atmospheric sciencesAmazonian[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencescomplex mixtureslcsh:ChemistryAtmospherechemistry.chemical_compoundparasitic diseasesCloud condensation nucleiSulfate0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category15. Life on landParticulateslcsh:QC1-999Trace gasAerosollcsh:QD1-999Volcanochemistry13. Climate actionEnvironmental sciencegeographic locationslcsh:Physics
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Microphysical Properties of Ice Crystal Precipitation and Surface-Generated Ice Crystals in a High Alpine Environment in Switzerland

2017

AbstractDuring the Cloud and Aerosol Characterization Experiment (CLACE) 2013 field campaign at the High Altitude Research Station Jungfraujoch, Switzerland, optically thin pure ice clouds and ice crystal precipitation were measured using holographic and other in situ particle instruments. For cloud particles, particle images, positions in space, concentrations, and size distributions were obtained, allowing one to extract size distributions classified by ice crystal habit. Small ice crystals occurring under conditions with a vertically thin cloud layer above and a stratocumulus layer approximately 1 km below exhibit similar properties in size and crystal habits as Antarctic/Arctic diamond …

Atmospheric Science010504 meteorology & atmospheric sciencesAtmospheric sciences01 natural sciencesPhysics::Geophysics010309 opticsDiamond dustSea ice growth processesCloud microphysics0103 physical sciencesIce fogPrecipitationCrystal habitComplex terrainPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesIce crystalsIce particlesSurface observations13. Climate actionIn situ atmospheric observationsIce nucleusParticleAstrophysics::Earth and Planetary Astrophysics/dk/atira/pure/subjectarea/asjc/1900/1902GeologyJournal of Applied Meteorology and Climatology
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