Search results for " resolution"

showing 10 items of 1159 documents

Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006

2009

The Saharan Mineral Dust Experiment (SAMUM) was conducted in May/June 2006 in southern Morocco. As part of SAMUM, airborne in situ measurements of the particle size distribution in the diameter range 4 nm < Dp < 100 μm were conducted. The aerosol mixing state was determined below Dp < 2.5 μm. Furthermore, the vertical structure of the dust layers was investigated with a nadir-looking high spectral resolution lidar (HSRL). The desert dust aerosol exhibited two size regimes of different mixing states: below 0.5 μm, the particles had a non-volatile core and a volatile coating; larger particles above 0.5 μm consisted of non-volatile components and contained light absorbing material. In…

Atmospheric ScienceRange (particle radiation)Materials science010504 meteorology & atmospheric sciencesgiant particlesAnalytical chemistryAtmosphärische Spurenstoffemixing state010501 environmental sciencesMineral dust01 natural sciencesAerosoldust layer structureTroposphereSAMUMdesert dustParticle-size distributionUltrafine particleParticle sizeparticle size distributionSpectral resolutionairborne measurements0105 earth and related environmental sciencesRemote sensingTellus B
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Developments for vegetation fluorescence retrieval from spaceborne high-resolution spectrometry in the O2-A and O2-B absorption bands

2010

Solar-induced chlorophyll fluorescence is a weak electromagnetic signal emitted in the red and far-red spectral regions by vegetation chlorophyll under excitation by solar radiation. Chlorophyll fluorescence has been demonstrated to be a close proxy to vegetation physiological functioning. The basis for fluorescence retrieval from passive space measurements is the exploitation of the O2-A and O2-B atmospheric absorption features to isolate the fluorescence signal from the solar radiation reflected by the surface and the atmosphere. High spectral resolution measurements and a precise modeling of the atmospheric radiative transfer in the visible and near-infrared regions are mandatory. Recent…

Atmospheric ScienceSoil ScienceAquatic ScienceRadiationOceanographychemistry.chemical_compoundOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferSpectral resolutionSpectroscopyChlorophyll fluorescenceEarth-Surface ProcessesWater Science and TechnologyRemote sensingEcologybusiness.industryPaleontologyForestryFluorescenceGeophysicschemistrySpace and Planetary ScienceAbsorption bandChlorophyllEnvironmental sciencebusinessJournal of Geophysical Research
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Aerosol closure study by lidar, sun photometry, and airborne optical counters during DAMOCLES field campaign at El Arenosillo sounding station, Spain

2011

We present a comparison of aerosol properties derived from in situ and remote sensing instruments during DAMOCLES campaign, aimed at investigating the equivalence between the instrumentation and methodologies employed by several Spanish groups to study atmospheric aerosols at a regional background site. The complete set of instruments available during this closure experiment allowed collecting a valuable high-resolution aerosol measurement data set. The data set was augmented with airborne in situ measurements carried out in order to characterize aerosol particles during the midday of 29 June 2006. This work is focused on aerosol measurements using different techniques of high-quality instr…

Atmospheric ScienceTeledeteccióSoil ScienceHigh resolutionAquatic ScienceOceanographycomplex mixturesPhotometry (optics)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Aerosol extinction coefficientField campaignEarth-Surface ProcessesWater Science and TechnologyRemote sensingAerosolsEcologyPaleontologyForestryGeofísicarespiratory systemRemote sensingAtmosphere -- Laser observationsAerosolBoundary layerDepth soundingAtmosfera -- Observacions amb làserGeophysicsLidar:Enginyeria de la telecomunicació::Radiocomunicació i exploració electromagnètica::Teledetecció [Àrees temàtiques de la UPC]Space and Planetary ScienceEnvironmental science:Desenvolupament humà i sostenible::Degradació ambiental::Contaminació atmosfèrica [Àrees temàtiques de la UPC]
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Early detection of volcanic hazard by lidar measurement of carbon dioxide

2016

Volcanic gases give information on magmatic processes. In particular, anomalous releases of carbon dioxide precede volcanic eruptions. Up to now, this gas has been measured in volcanic plumes with conventional measurements that imply the severe risks of local sampling and can last many hours. For these reasons and for the great advantages of laser sensing, the thorough development of volcanic lidars has been undertaken at ENEA (Italian National Agency for New Technologies, Energy and Sustainable Economic Development). In fact, lidar profiling allows one to scan remotely volcanic plumes in a fast and continuous way, and with high spatial and temporal resolution. A differential absorption lid…

Atmospheric ScienceVolcanic hazardsGas detection02 engineering and technology01 natural scienceslaw.invention010309 opticsVolcanic Gases020210 optoelectronics & photonicsImpact craterlawNatural hazard0103 physical sciences0202 electrical engineering electronic engineering information engineeringEarth and Planetary Sciences (miscellaneous)eventWater Science and TechnologyRemote sensingevent.disaster_typegeographygeography.geographical_feature_categoryVolcanic hazardLaserLaser remote sensingLidarDifferential absorption lidarVolcano13. Climate actionTemporal resolutionGeologyNatural Hazards
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Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006

2009

During the Saharan Mineral Dust Experiment (SAMUM) conducted in summer 2006 in southeast Morocco, the complex refractive index of desert dust was determined from airborne measurements of particle size distributions and aerosol absorption coefficients at three different wavelengths in the blue (467 nm), green (530 nm) and red (660 nm) spectral regions. The vertical structure of the dust layers was analysed by an airborne high spectral resolution lidar (HSRL). The origin of the investigated dust layers was estimated from trajectory analyses, combined with Meteosat 2nd Generation (MSG) scenes and wind field data analyses. The real part n of the dust refractive index was found almost constant w…

Atmospheric Sciencerefractive indexMaterials science010504 meteorology & atmospheric sciencesaerosolAtmosphärische SpurenstoffeMineralogy010501 environmental sciencesMineral dust01 natural sciencesAerosolSAMUMTroposphereWavelengthLidarSpectral resolutionAbsorption (electromagnetic radiation)absorptionRefractive index0105 earth and related environmental sciencesRemote sensingTellus B: Chemical and Physical Meteorology
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Analysis of broadband surface BRDFs derived from TOA SW CERES measurements for surfaces classified by the IGBP land cover

2012

Most studies on the reflectance properties of the Earth's surface are addressed estimating the bidirectional reflectance distribution function (BRDF) of high spatial resolution and high spectral resolution satellite measurements. This article assesses the development of broadband (BB) BRDFs from radiances corresponding to large footprints classified according to the International Geosphere-Biosphere Programme (IGBP) land-cover classification. Top-of-atmosphere (TOA) shortwave (SW) CERES (Clouds and the Earth's Radiant Energy System) measurements are employed to invert the bidirectional reflectance factor (BRF) Rahman–Pinty–Verstraete (RPV) model for regions identified with the same IGBP typ…

Atmospheric radiative transfer codesComputationParametric modelGeneral Earth and Planetary SciencesRadiant energyEnvironmental scienceBidirectional reflectance distribution functionLand coverSpectral resolutionAtmospheric sciencesShortwaveRemote sensingInternational Journal of Remote Sensing
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High-resolution Fourier transform infrared spectroscopy and analysis of the ν3 fundamental band of P4

1999

Abstract We present the first high-resolution infrared absorption study of the ν 3 fundamental of white phosphorus, P 4 . This spectrum has been analyzed using the STDS (Spherical Top Data System) software. The band center lies at 466.286 cm −1 . With the approximation ( Bζ ) 3 =− B 0 /2, we found that the ground-state bond length is r 0 =219.58 pm. This value is consistent with that of ab initio studies reported previously but significantly different from a value obtained from a Raman study.

Bond lengthsymbols.namesakeChemistryAnalytical chemistryAb initiosymbolsGeneral Physics and AstronomyInfrared spectroscopyHigh resolutionPhysical and Theoretical ChemistryFourier transform infrared spectroscopyRaman spectroscopyFourier transform spectroscopyChemical Physics Letters
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A method to reduce the FP/imm number through CC and MLO views comparison in mammographic images

2008

In this paper we propose a method to reduce the FP/imm number through CC and MLO mammographic views comparison of the same patient. The proposed solution uses the symmetry properties of the breast to compute a geometric transformation that permits to represent the two images in comparable coordinates systems. Through this method, potential pathological ROIs of one of the projections are correlated with the ROIs in the second view. To show the effectiveness of the result we apply the method on a dataset composed of 112 couples of pathological images. Experiments shows that method enables a reduction by up to 700/0 of the FP/imm number detected after the classification step

Breast tissueData setbusiness.industryPathological imageGeometric transformationPattern recognitionSymmetry propertiesReduction (complexity)CorrelationMedical imagingMedicineArtificial intelligenceNuclear medicinebusinessGeometric transformationImage resolutionTransformation geometryMammographicMammographic image2008 IEEE Nuclear Science Symposium Conference Record
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First M87 Event Horizon Telescope Results. IV. Imaging the Central Supermassive Black Hole

2019

We present the first Event Horizon Telescope (EHT) images of M87, using observations from April 2017 at 1.3 mm wavelength. These images show a prominent ring with a diameter of ~40 μas, consistent with the size and shape of the lensed photon orbit encircling the "shadow" of a supermassive black hole. The ring is persistent across four observing nights and shows enhanced brightness in the south. To assess the reliability of these results, we implemented a two-stage imaging procedure. In the first stage, four teams, each blind to the others' work, produced images of M87 using both an established method (CLEAN) and a newer technique (regularized maximum likelihood). This stage allowed us to av…

Brightness010504 meteorology & atmospheric sciencesgalaxies: jetAstronomyblack hole physicsFOS: Physical sciencesgalaxies: individualtechniques: image processingAstrophysicsGeneral Relativity and Quantum Cosmology (gr-qc)galaxies: individual: M8701 natural sciencesSynthetic dataGeneral Relativity and Quantum Cosmologygalaxies: individual (M87)0103 physical sciencesimage processing [Techniques]010303 astronomy & astrophysicsInstrumentation and Methods for Astrophysics (astro-ph.IM)0105 earth and related environmental sciencesEvent Horizon TelescopePhysicsGround truthSupermassive black holetechniques: high angular resolutionAstronomy and AstrophysicsBlack hole physicsgalaxies: jetsindividual (M87) [Galaxies]Astrophysics - Astrophysics of Galaxiesblack hole physic3. Good healthOrbitInterferometryhigh angular resolution [Techniques]Space and Planetary Sciencetechniques: interferometricAstrophysics of Galaxies (astro-ph.GA)interferometric [Techniques]jets [Galaxies]Deconvolution[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]Astrophysics - Instrumentation and Methods for Astrophysics
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Imation of land surface emissivity differences in the split-window channels of AVHRR

1994

Abstract A method for estimating the difference between the channel emissivities in NOAA-AVHRR Channels 4 and 5 is proposed and applied to a data set from the HAPEX-MOBILHY experiment. The method is based on the separation between the atmospheric and emissivity effects in the brightness temperature difference measured with AVHRR Channels 4 and 5. Atmospheric profiles coincident to the satellite overpass and a radiative transfer model are required to estimate the atmospheric correction for brightness temperatures. With this procedure, the emissivity difference Δe is obtained at the satellite spatial and spectral resolution, which has a great interest for correcting thermal images with the sp…

BrightnessAtmospheric correctionSoil ScienceGeologyAtmospheric radiative transfer codesCoincidentBrightness temperatureEmissivityAstrophysics::Solar and Stellar AstrophysicsEnvironmental scienceSatelliteComputers in Earth SciencesSpectral resolutionPhysics::Atmospheric and Oceanic PhysicsRemote sensingRemote Sensing of Environment
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