Search results for "Size distributions"

showing 6 items of 6 documents

Intercomparison and evaluation of global aerosol microphysical properties among AeroCom models of a range of complexity

2014

Many of the next generation of global climate models will include aerosol schemes which explicitly simulate the microphysical processes that determine the particle size distribution. These models enable aerosol optical properties and cloud condensation nuclei (CCN) concentrations to be determined by fundamental aerosol processes, which should lead to a more physically based simulation of aerosol direct and indirect radiative forcings. This study examines the global variation in particle size distribution simulated by 12 global aerosol microphysics models to quantify model diversity and to identify any common biases against observations. Evaluation against size distribution measurements from…

Atmospheric Science010504 meteorology & atmospheric sciencesParticle numbergeneral-circulation modelmixing state010501 environmental sciencesEnvironmentclimate modelblack carbonAtmospheric sciences01 natural sciencesTropospherelcsh:ChemistryZeppelinobservatorietUrban Developmentddc:550Cloud condensation nucleiBuilt Environmentnumber size distributionsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMicrophysicsparticle formationEarth / EnvironmentalCloud physicsatmospheric aerosolCAS - Climate Air and SustainabilityRadiative forcinglcsh:QC1-999Aerosolcloud condensation nucleimarine boundary-layerlcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceClimate modelELSS - Earth Life and Social Sciencesoff-line modellcsh:Physics
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Pareto or log-normal? Best fit and truncation in the distribution of all cities

2015

In the literature, the distribution of city size is a controversial issue with two common contenders: the Pareto and the log-normal. While the first is most accredited when the distribution is truncated above a certain threshold, the latter is usually considered a better representation for the untruncated distribution of all cities. In this paper, we reassess the empirical evidence on the best-fitting distribution in relation to the truncation point issue. Specifically, we provide a comparison among four recently proposed approaches and alternative definitions of U.S. cities. Our results highlight the importance to look at issue of the best-fitting distribution together with the truncation …

City size distributions Pareto Log-Normal Truncation pointSettore SECS-P/06 - Economia Applicata
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Validity of NMR pore-size analysis of cultutal heritage ancient building materials containing magnetic impurities

2007

NMR relaxation time distributions, obtained with laboratory and portable devices, are utilized to characterize the pore-size distributions of building materials coming from the Roman remains of the Greek-Roman Theatre of Taormina. To validate the interpretation of relaxation data in terms of pore-size distribution, comparison of results from standard and in situ NMR experiments with results of the mercury intrusion porosimetry (MIP) has been made. Although the pore-size distributions can be obtained by NMR in terms of either longitudinal (T-1) or transverse (T-2) relaxation times distributions, the shorter duration of the T-2 measurement makes it, in principle, preferable, although the dete…

Pore sizeNuclear and High Energy PhysicsNMR porosimetryPOROUS-MEDIAMineralogyGRADIENTSNMR building materialsSingle-sided NMRImpurityPORE-SIZE DISTRIBUTIONSStatistical physicsInstrumentationNMR porous mediaRadiationChemistryIN SITU ANALYSISRelaxation (NMR)nmr building materials; nmr cultural heritage; nmr porosimetry; nmr porous media; nmr relaxation; pore-size distribution; single-sided nmr; taormina theatrePOROUS MEDIANMR cultural heritageGeneral ChemistryRESONANCENmr dataFIELDSDIFFUSIONNMRMagnetic fieldPore-size distributionCultural heritageDistribution (mathematics)Taormina TheatreNMR relaxationCULTURAL HERITAGEMercury intrusion porosimetry
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Nuclear Magnetic Resonance for Cultural Heritage

2007

Abstract Nuclear magnetic resonance (NMR) portable devices are now being used for nondestructive in situ analysis of water content, pore space structure and protective treatment performance in porous media in the field of cultural heritage. It is a standard procedure to invert T 1 and T 2 relaxation data of fully water-saturated samples to get “pore size” distributions, but the use of T 2 requires great caution. It is well known that dephasing effects due to water molecule diffusion in a magnetic field gradient can affect transverse relaxation data, even if the smallest experimentally available half echo time τ is used in Carr–Purcell–Meiboom–Gill experiments. When a portable single-sided N…

Single-sided NMR deviceGeologic SedimentsPORE SIZE DISTRIBUTIONSMagnetic Resonance SpectroscopyTime FactorsField (physics)Scale (ratio)Surface PropertiesSample (material)DiffusionDephasingBiomedical EngineeringBiophysicsInhomogeneous magnetic fieldsDiffusionNuclear magnetic resonanceRadiology Nuclear Medicine and imagingNMR SINGLE-SIDEDChemistryConstruction MaterialsRelaxation (NMR)WaterPOROUS MEDIANMRArchaeologyNMR relaxationNuclear magnetic resonance in porous mediaPorous mediaNMR relaxationSingle-sided NMR deviceInhomogeneous magnetic fieldsCultural heritageCULTURAL HERITAGEPorous mediumPorosity
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A particle based simulation model for glacier dynamics

2013

This publication is contribution number 22 of the Nordic Centre of Excellence SVALI, “Stability and Variations of Arctic Land Ice”, funded by the Nordic Top-level Research Initiative (TRI). The work has been supported by the SVALI project through the University of Lapland, Arctic Centre, and through the University Centre in Svalbard. Funding was also provided by the Conoco-Phillips and Lunding High North Research Program (CRIOS: Calving Rates and Impact on Society). A particle-based computer simulation model was developed for investigating the dynamics of glaciers. In the model, large ice bodies are made of discrete elastic particles which are bound together by massless elastic beams. These…

business.product_categoryGlacier terminusTidewater glaciersBasal conditionsLaskennallinen materiaalifysiikkaCalving glaciersPhysics::GeophysicsBergy bitsDiscrete element modelG1SDG 14 - Life Below WaterInclined planefysiikkaGeomorphologylcsh:Environmental sciencesPhysics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and Technologylcsh:GE1-350ice behaviourgeographygeography.geographical_feature_categorymekaniikkaIce-sheetIcebergslcsh:QE1-996.5Computational material physicsjään tutkimusGlacierG Geography (General)MechanicsDebrisIcebergFinite element methodMassless particlelcsh:GeologyHydrodynamicsIce sheetSize distributionsbusinessStabilityGeology
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ESTIMATING RAINFALL EROSIVITY BY DROP SIZE DISTRIBUTIONS

Water soil erosion is a process of detachment and transport of soil particles due to rainfall and runoff and it is the main cause of the modeling of extended portions of the earth's surface. The acceleration of the process through anthropogenic perturbation has severe impacts on soil and environmental quality. Soil erosion above a certain level will reduce soil productivity over the long haul. It exposes subsoil, which has often poor qualities for crop establishment and growth, and it can lead to stand loss by sediment deposition. A fundamental property of rainfall for understanding how it is made up is the raindrop size distribution (DSD). The knowledge of the raindrop size distribution at…

rainfall intensityrainfall kinetic powerSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliRainfall erosivitydrop size distributions
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