Search results for "Geophysics"

showing 10 items of 2645 documents

A multi-instrument approach for characterizing the atmospheric aerosol optical thickness during the STAAARTE/DAISEX-99 campaign

2002

This work deals with the retrieval of the aerosol optical thickness (AOT) needed to carry out the atmospheric correction of remote sensing data measured in Barrax (Spain) on 4 June 1999 in the framework of 1999 Digital Airbone Imaging Spectrometer Experiment (DAISEX'99). The AOT was estimated through three approaches based on: spectral extinction of direct solar irradiance at ground level, airborne nephelometer measurements at different altitudes, and backscatter lidar in the lower troposphere. We found extremely low AOT values due to a cold Atlantic front that swept across the Iberian Peninsula from west to east producing light rain over the test area on 2 June 1999. The results were solar…

NephelometerBackscatterSingle-scattering albedoAtmospheric correctionImaging spectrometerGeofísicaSolar irradianceAtmospheric sciencesSpectrometerGeophysicsLidarExtinction (optical mineralogy)Aerosol optical thicknessGeneral Earth and Planetary SciencesEnvironmental scienceAtmospheric aerosolRemote sensing
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Clues to the nature of the impacting bodies from platinum-group elements (rhenium and gold) in borehole samples from the Clearwater East crater (Cana…

1997

— Seven large (10 g) impact melt rock samples from boreholes from the Boltysh impact crater (Ukraine) and six samples from the East Clearwater crater (Canada) were analyzed for Os, Ir, Ru, Rh, Pd, Re and Au by the nickel sulfide technique in combination with neutron activation. Earlier analyses of Clearwater East impact melt rocks have shown that they are strongly enriched in Ir, Os, Pd and Re. In this work, I confirm earlier findings and demonstrate similarly high enrichments of Rh and Ru. The average Os/Ir, Ru/Ir, Pd/Ir, Rh/Ir and Ru/Rh ratios of the melt rock samples from Clearwater East are CI-chondritic and yield an average Ir content of 25.2 ± 6.5 ng/g relative to an average upper cru…

Nickel sulfideBoreholeMineralogychemistry.chemical_elementRheniumPlatinum groupchemistry.chemical_compoundGeophysicsImpact craterchemistrySpace and Planetary ScienceUpper crustRefractory (planetary science)GeologyNeutron activationMeteoritics & Planetary Science
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Mn, Fe, Zn and As speciation in a fast-growing ferromanganese marine nodule

2004

The speciation of Mn, Fe, As and Zn in a fast-growing (0.02mm/yr), shallow-marine ferromanganese nodule has been examined by micro X-ray fluorescence, micro X-ray diffraction, and micro X-ray absorption spectroscopy. This nodule exhibits alternating Fe-rich and Mn-rich layers reflecting redox variations in water chemistry. Fe occurs as two-line ferrihydrite. The As is strictly associated with Fe and is mostly pentavalent, with an environment similar to that of As sorbed on or coprecipitated with synthetic ferrihydrite. The Mn is in the form of turbostratic birnessite with ~;10 percent trivalent manganese in the layers and probably ~;8 percent corner-sharing metal octahedra in the interlayer…

Nodule (geology)BirnessiteXASInorganic chemistrychemistry.chemical_elementManganese010501 environmental sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesFerromanganeseMetalFerrihydriteXAS EXAFS marine ferromanganese nodule Baltic sea speciation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and Petrology0105 earth and related environmental sciencesX-ray absorption spectroscopyBaltic seaExtended X-ray absorption fine structureRadiochemistrymarine ferromanganese nodule6. Clean waterEXAFSspeciationchemistryvisual_artEarth Sciencesvisual_art.visual_art_mediumengineeringEnvironmental scienceGeochimica et Cosmochimica Acta
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Characteristics of seasonal variations and noises of the daily double-difference and PPP solutions

2020

Abstract Long term GNSS observations provided by networks of the continuously operating reference stations (CORS) allow for determination of the global and local tectonic plate movements and seasonal variations. In recent years, PPP (Precise Point Positioning) technique has become increasingly popular and most likely in the future will replace relative positioning with CORS stations. In this paper, we discuss the difference of the velocity and seasonal component estimates of 25 Latvian CORS stations on the basis of daily PPP solutions from the Nevada Geodetic Laboratory and double-difference solutions from the Institute of Geodesy and Geoinformatics of the University of Latvia. Time series …

Noise010504 meteorology & atmospheric sciencesDouble differenceModeling and SimulationAcousticsEarth and Planetary Sciences (miscellaneous)010502 geochemistry & geophysics01 natural sciencesEngineering (miscellaneous)Geology0105 earth and related environmental sciencesJournal of Applied Geodesy
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Geodynamic inversion to constrain the non-linear rheology of the lithosphere

2015

A common method to determine the strength of the lithosphere is through estimating its effective elastic thickness from the coherence between gravity and topography. This method assumes a priori that the lithosphere is a thin elastic plate floating on a viscous mantle. Whereas this seems to work well with oceanic plates, it has given controversial results in continental collision zones. Usually, continental collisions zones are well-studied areas for which additional geophysical datasets such as receiver functions and seismic tomography exist that constrain the geometry of the lithosphere and often show that it is rather complex. Yet, lithospheric geometry by itself is insufficient to under…

Nonlinear systemGeophysicsRheologyContinental collisionGeochemistry and PetrologyOceanic crustLithosphereSeismic tomographyGeophysicsGeologyMantle (geology)Physics::GeophysicsCoherence (physics)Geophysical Journal International
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On a new robust workflow for the statistical and spatial analysis of fracture data collected with scanlines (or the importance of stationarity)

2020

Abstract. We present an innovative workflow for the statistical analysis of fracture data collected along scanlines, composed of two major stages, each one with alternative options. A prerequisite in our analysis is the assessment of stationarity of the dataset, which is motivated by statistical and geological considerations. Calculating statistics on non-stationary data can be statistically meaningless, and moreover the normalization and/or sub-setting approach that we discuss here can greatly improve our understanding of geological deformation processes. Our methodology is based on performing non-parametric statistical tests, which allow detecting important features of the spatial distrib…

Normalization (statistics)statistical and spatial analysis of fracture dataComputer scienceStratigraphylcsh:QE1-996.5PaleontologySoil ScienceGeologyFunction (mathematics)computer.software_genrelcsh:GeologyGeophysicsWorkflowlcsh:StratigraphyGeochemistry and PetrologyFracture (geology)Statistical analysisData miningSpatial analysiscomputerlcsh:QE640-699Earth-Surface ProcessesSolid Earth
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Revising midlatitude summer temperatures back to A.D. 600 based on a wood density network

2015

Annually resolved and millennium-long reconstructions of large-scale temperature variability are primarily composed of tree ring width (TRW) chronologies. Changes in ring width, however, have recently been shown to bias the ratio between low- and high-frequency signals. To overcome limitations in capturing the full spectrum of past temperature variability, we present a network of 15 maximum latewood density (MXD) chronologies distributed across the Northern Hemisphere extratropics. Independent subsets of continental-scale records consistently reveal high MXD before 1580 and after 1910, with below average values between these periods. Reconstructed extratropical summer temperatures reflect n…

Northern HemisphereTree ringsClimate changeG Geography (General)Dendroclimatology3rd-DASAtmospheric sciencesAtmosphereMaximum latewood densityVolcanic coolingGeophysicsMillennial reconstructionMiddle latitudesClimatologyPaleoclimatologyG1Extratropical cycloneDendrochronologyLittle Ice AgeGeneral Earth and Planetary SciencesBeta valueGeology
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Measurement of South Pole ice transparency with the IceCube LED calibration system

2013

The IceCube Neutrino Observatory, approximately 1 km^3 in size, is now complete with 86 strings deployed in the Antarctic ice. IceCube detects the Cherenkov radiation emitted by charged particles passing through or created in the ice. To realize the full potential of the detector, the properties of light propagation in the ice in and around the detector must be well understood. This report presents a new method of fitting the model of light propagation in the ice to a data set of in-situ light source events collected with IceCube. The resulting set of derived parameters, namely the measured values of scattering and absorption coefficients vs. depth, is presented and a comparison of IceCube …

Nuclear and High Energy PhysicsPhysics - Instrumentation and DetectorsSouth Pole icePhoton progagationAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesAstrophysicsddc:500.201 natural sciencesHigh Energy Physics - ExperimentIceCube Neutrino ObservatoryIceCubePhysics::GeophysicsHigh Energy Physics - Experiment (hep-ex)0103 physical sciencesCalibrationddc:53014. Life underwater010306 general physicsAbsorption (electromagnetic radiation)InstrumentationInstrumentation and Methods for Astrophysics (astro-ph.IM)Cherenkov radiationRemote sensingPhysicsOptical properties010308 nuclear & particles physicsScatteringDetectorAstrophysics::Instrumentation and Methods for AstrophysicsIceCube; Optical properties; Photon propagation; South Pole iceSouth PoleiceInstrumentation and Detectors (physics.ins-det)Charged particleData setPhoton propagationAstrophysics - Instrumentation and Methods for AstrophysicsNuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
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If sterile neutrinos exist, how can one determine the total solar neutrino fluxes?

2002

The 8B solar neutrino flux inferred from a global analysis of solar neutrino experiments is within 11% (1 sigma) of the predicted standard solar model value if only active neutrinos exist, but could be as large as 1.7 times the standard prediction if sterile neutrinos exist. We show that the total 8B neutrino flux (active plus sterile neutrinos) can be determined experimentally to about 10% (1 sigma) by combining charged current measurements made with the KamLAND reactor experiment and with the SNO CC solar neutrino experiment, provided the LMA neutrino oscillation solution is correct and the simulated performance of KamLAND is valid. Including also SNO NC data, the sterile component of the…

Nuclear and High Energy PhysicsSterile neutrinoParticle physicsAstrofísica nuclearNuclear TheoryPhysics::Instrumentation and DetectorsSolar neutrinoAstrophysics::High Energy Astrophysical PhenomenaSolar neutrinosFOS: Physical sciencesAstrophysics01 natural sciences7. Clean energyHigh Energy Physics - ExperimentPhysics::GeophysicsNuclear Theory (nucl-th)Nuclear physicsHigh Energy Physics - Experiment (hep-ex)High Energy Physics - Phenomenology (hep-ph)Neutrins solars0103 physical sciencesNuclear Experiment (nucl-ex)010306 general physicsNeutrino oscillationNuclear ExperimentBorexinoPhysics010308 nuclear & particles physicsAstrophysics (astro-ph)High Energy Physics::PhenomenologyFísicaSolar neutrino problemHigh Energy Physics - PhenomenologyNeutrino detectorMeasurements of neutrino speedHigh Energy Physics::ExperimentNuclear astrophysicsNeutrino
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External ballistic of volcanic explosions

1983

In order to determine the kinetic energy of an explosion it is necessary to know the initial velocities of ejected fragments. Calculations of initial velocities made earlier with few exceptions did not take into account the resistance of the air and therefore, greatly underestimated the initial velocities, and consequently the energy of the explosions. A solution of the inverse problem of ballistics which takes into account air resistance makes it possible to find precise values of initial velocities of ejection, determined from the distance of ejected fragments and their ballistic coefficients. The method makes it possible to determine the kinetic energy of explosions for eruptions which w…

Nuclear explosionVulcanian eruptionExplosive eruptionBallisticsVolcanismMechanicsGeophysicsKinetic energyGeochemistry and PetrologyDragPhysics::Space PhysicsAstrophysics::Solar and Stellar AstrophysicsEjectaGeologyBulletin Volcanologique
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