Search results for "CONDENSATION"

showing 10 items of 468 documents

Airborne measurements of the nitric acid partitioning in persistent contrails

2009

This study reports the first systematic measurements of nitric acid (HNO3) uptake in contrail ice particles at typical aircraft cruise altitudes. During the CIRRUS-III campaign cirrus clouds and almost 40 persistent contrails were probed with in situ instruments over Germany and Northern Europe in November 2006. Besides reactive nitrogen, water vapor, cloud ice water content, ice particle size distributions, and condensation nuclei were measured during 6 flights. Contrails with ages up to 12 h were detected at altitudes 10–11.5 km and temperatures 211–220 K. These contrails had a larger ice phase fraction of total nitric acid (HNO3ice/HNO3tot = 6%) than the ambient cirrus layers (3%). On av…

Atmospheric ScienceReactive nitrogencontrailsAtmosphärische SpurenstoffecirrusAtmospheric scienceslcsh:QC1-999Plumelcsh:Chemistrychemistry.chemical_compoundlcsh:QD1-999chemistryNitric acidPhase (matter)uptakepartitioningEnvironmental scienceCloud condensation nucleiCirrusParticle sizeNitric acidaircraft measurementslcsh:PhysicsWater vapor
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Irreversible loss of ice nucleation active sites in mineral dust particles caused by sulphuric acid condensation

2010

Abstract. During the FROST-2 (FReezing Of duST) measurement campaign conducted at the Leipzig Aerosol Cloud Interaction Simulator (LACIS), we investigated changes in the ice nucleation properties of 300 nm Arizona Test Dust mineral particles following thermochemical processing by varying amounts and combinations of exposure to sulphuric acid vapour, ammonia gas, water vapour, and heat. The processed particles' heterogeneous ice nucleation properties were determined in both the water subsaturated and supersaturated humidity regimes at −30 °C and −25 °C using Colorado State University's continuous flow diffusion chamber. The amount of sulphuric acid coating material was estimated by an aeroso…

Atmospheric ScienceSupersaturation010504 meteorology & atmospheric sciencesChemistryCondensationHumidityMineralogy010501 environmental sciencesMineral dust01 natural scienceslcsh:QC1-999respiratory tract diseasesAerosollcsh:Chemistrylcsh:QD1-999Chemical engineering13. Climate actionIce nucleusDissolutionlcsh:PhysicsWater vapor0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Aerosol physicochemical effects on CCN activation simulated with the chemistry-climate model EMAC

2017

Abstract This study uses the EMAC atmospheric chemistry-climate model to simulate cloud properties with a prognostic cloud droplet nucleation scheme. We present modeled global distributions of cloud condensation nuclei (CCN) number concentrations and CCN activation rates, together with the effective hygroscopicity parameter κ, to describe the aerosol chemical composition effect on CCN activation. Large particles can easily activate into cloud droplets, even at low κ values due to the dominant size effect in cloud droplet formation. Small particles are less efficiently activated as CCN, and are more sensitive to aerosol composition and supersaturation. Since the dominant fraction of small pa…

Atmospheric ScienceSupersaturation010504 meteorology & atmospheric sciencesChemistrybusiness.industryNorthern HemisphereNucleationCloud computing010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesAerosolAtmosphereClimatologyCloud condensation nucleibusinessChemical composition0105 earth and related environmental sciencesGeneral Environmental ScienceAtmospheric Environment
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The ice nucleating ability of pollen

2001

Abstract Laboratory experiments are described where the water uptake by a variety of pollen was studied quantitatively, followed by the investigation of the ice nucleating ability of four kinds of pollen in the deposition and the condensation freezing modes. The diameters of the pollen selected for the freezing experiments were between 25 and 70 μm. The freezing experiments in the deposition mode including also pollen resuspended from decayed leaves, and crushed pollen grains were carried out at different temperatures down to −33 °C combined with various supersaturations with respect to ice up to 35%. The condensation freezing experiments were carried out at temperatures down to −18 °C at s…

Atmospheric ScienceSupersaturationChemistryCapillary actionCondensationAnalytical chemistryMineralogymedicine.disease_causePollenCongelationmedicineIce nucleusCloud condensation nucleiDeposition (chemistry)Atmospheric Research
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2009

Abstract. We have investigated the formation of cloud droplets under pyro-convective conditions using a cloud parcel model with detailed spectral microphysics and with the κ-Kohler model approach for efficient and realistic description of the cloud condensation nucleus (CCN) activity of aerosol particles. Assuming a typical biomass burning aerosol size distribution (accumulation mode centred at 120 nm), we have calculated initial cloud droplet number concentrations (NCD) for a wide range of updraft velocities (w=0.25–20 m s−1) and aerosol particle number concentrations (NCN=200–105 cm−3) at the cloud base. Depending on the ratio between updraft velocity and particle number concentration (w/…

Atmospheric ScienceSupersaturationMicrophysicsParticle numberChemistryParticle-size distributionAnalytical chemistryCloud condensation nucleiParticleAtmospheric sciencesWater vaporAerosolAtmospheric Chemistry and Physics
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Nucleation in physical and nonphysical systems

2003

Abstract The aggregation of particles out of an initially homogeneous situation is well known in physics. Depending on the system under consideration and its control parameters, the cluster formation in a supersaturated (metastable or unstable) situation has been observed in nucleation physics as well as in other branches. We investigate the well-known example of condensation (formation of liquid droplets) in an undercooled vapour to conclude that the formation of bound states as a phase transition is related to transportation science. We present a comparison of nucleation in an isothermal–isochoric container with traffic congestion on a circular one-lane freeway. The analysis is based, in …

Atmospheric ScienceSupersaturationPhase transitionMaterials scienceMetastabilityCondensationMaster equationBound stateCluster (physics)NucleationMechanicsAtmospheric Research
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Mechanisms of Banner Cloud Formation

2013

Abstract Banner clouds are clouds in the lee of steep mountains or sharp ridges. Their formation has previously been hypothesized as due to three different mechanisms: (i) vertical uplift in a lee vortex (which has a horizontal axis), (ii) adiabatic expansion along quasi-horizontal trajectories (the so-called Bernoulli effect), and (iii) a mixing cloud (i.e., condensation through mixing of two unsaturated air masses). In the present work, these hypotheses are tested and quantitatively evaluated against each other by means of large-eddy simulation. The model setup is chosen such as to represent idealized but prototypical conditions for banner cloud formation. In this setup the lee-vortex mec…

Atmospheric ScienceWork (thermodynamics)Meteorologymedia_common.quotation_subjectCondensationGeometryAsymmetryPlumeVortexBernoulli's principleAdiabatic processMixing (physics)Geologymedia_commonJournal of the Atmospheric Sciences
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2012

Abstract. We present a numerical modelling study investigating the impact of mineral dust on cloud formation over the Eastern Mediterranean for two case studies: (i) 25 September 2008 and (ii) 28/29 January 2003. In both cases dust plumes crossed the Mediterranean and interacted with clouds forming along frontal systems. For our investigation we used the fully online coupled model WRF-chem. The results show that increased aerosol concentrations due to the presence of mineral dust can enhance the formation of ice crystals. This leads to slight shifts of the spatial and temporal precipitation patterns compared to scenarios where dust was not considered to act as ice nuclei. However, the total…

Atmospheric Scienceeducation.field_of_study010504 meteorology & atmospheric sciencesIce crystalsPopulation010501 environmental sciencesRadiative forcingMineral dustAtmospheric sciencescomplex mixtures01 natural sciences13. Climate actionClimatologyIce nucleusEnvironmental scienceCloud condensation nucleisense organsPrecipitationeducation0105 earth and related environmental sciencesOrographic liftAtmospheric Chemistry and Physics
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Characterization of the inter-annual, seasonal, and diurnal variations of condensation particle concentrations at Neumayer, Antarctica

2011

Continuous condensation particle (CP) observations were conducted from 1984 through 2009 at Neumayer Station under stringent contamination control. During this period, the CP concentration (median 258 cm<sup>−3</sup>) showed no significant long term trend but exhibited a pronounced seasonality characterized by a stepwise increase starting in September and reaching its annual maximum of around 10<sup>3</sup> cm<sup>−3</sup> in March. Minimum values below 10<sup>2</sup> cm<sup>–3</sup> were observed during June/July. Dedicated time series analyses in the time and frequency domain revealed no significant correlations between…

Atmospheric Sciencefood.ingredient010504 meteorology & atmospheric sciencesAtmospheric circulationaerosolnon-volatile particles010501 environmental sciencesAtmospheric sciences01 natural scienceslcsh:ChemistryfoodUltrafine particlecondensation particlesmedicine14. Life underwater0105 earth and related environmental sciencesVulcanian eruptionSea saltCondensationAtmosphärische SpurenstoffeNeumayerSeasonalitymedicine.diseaselcsh:QC1-999Aerosollcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceParticlelcsh:PhysicsAtmospheric Chemistry and Physics
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2009

Abstract. A characterization of the ultra-fine aerosol particle counter COPAS (COndensation PArticle counting System) for operation on board the Russian high altitude research aircraft M-55 Geophysika is presented. The COPAS instrument consists of an aerosol inlet and two dual-channel continuous flow Condensation Particle Counters (CPCs) operated with the chlorofluorocarbon FC-43. It operates at pressures between 400 and 50 hPa for aerosol detection in the particle diameter (dp) range from 6 nm up to 1 μm. The aerosol inlet, designed for the M-55, is characterized with respect to aspiration, transmission, and transport losses. The experimental characterization of counting efficiencies of th…

Atmospheric SciencegeographyRange (particle radiation)geography.geographical_feature_categoryChemistryCondensationAnalytical chemistryParticleInletParticle counterCondenser (heat transfer)AerosolLine (formation)Atmospheric Measurement Techniques
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