Search results for "clou"

showing 10 items of 830 documents

Effects of 20–100 nm particles on liquid clouds in the clean summertime Arctic

2016

Abstract. Observations addressing effects of aerosol particles on summertime Arctic clouds are limited. An airborne study, carried out during July 2014 from Resolute Bay, Nunavut, Canada, as part of the Canadian NETCARE project, provides a comprehensive in situ look into some effects of aerosol particles on liquid clouds in the clean environment of the Arctic summer. Median cloud droplet number concentrations (CDNC) from 62 cloud samples are 10 cm−3 for low-altitude cloud (clouds topped below 200 m) and 101 cm−3 for higher-altitude cloud (clouds based above 200 m). The lower activation size of aerosol particles is  ≤  50 nm diameter in about 40 % of the cases. Particles as small as 20 nm ac…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesClean environment010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999The arcticAerosollcsh:ChemistryArcticlcsh:QD1-99913. Climate actionLiquid water contentAerosol cloudClimatologyCloud condensation nucleiEnvironmental sciencelcsh:Physics0105 earth and related environmental sciences
researchProduct

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
researchProduct

Apparent absorption of solar spectral irradiance in heterogeneous ice clouds

2010

[1] Coordinated flight legs of two aircraft above and below extended ice clouds played an important role in the Tropical Composition, Cloud and Climate Coupling Experiment (Costa Rica, 2007). The Solar Spectral Flux Radiometer measured up- and downward irradiance on the high-altitude (ER-2) and the low-altitude (DC-8) aircraft, which allowed deriving apparent absorption on a point-by-point basis along the flight track. Apparent absorption is the vertical divergence of irradiance, calculated from the difference of net flux at the top and bottom of a cloud. While this is the only practical method of deriving absorption from aircraft radiation measurements, it differs from true absorption when…

Atmospheric ScienceSpectral shape analysisIrradianceSoil ScienceAquatic ScienceOceanographyice cloud absorptionAtmosphereAtmospheric radiative transfer codesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)3-D radiative transferAbsorption (electromagnetic radiation)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and TechnologyRemote sensingPhysicsEffective radiusRadiometerEcologyFernerkundung der AtmosphärePaleontologyForestryGeophysicsSpace and Planetary Sciencesolar spectral measurementsModerate-resolution imaging spectroradiometer
researchProduct

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
researchProduct

2018

Abstract. The growth of small cloud droplets and ice crystals is dominated by the diffusion of water vapor. Usually, Maxwell's approach to growth for isolated particles is used in describing this process. However, recent investigations show that local interactions between particles can change diffusion properties of cloud particles. In this study we develop an approach for including these local interactions into a bulk model approach. For this purpose, a simplified framework of local interaction is proposed and governing equations are derived from this setup. The new model is tested against direct simulations and incorporated into a parcel model framework. Using the parcel model, possible i…

Atmospheric ScienceSupersaturation010504 meteorology & atmospheric sciencesIce crystalsbusiness.industryCloud computingMechanicsAtmospheric sciencesFluid parcel01 natural sciences010305 fluids & plasmasScientific method0103 physical sciencesCloud dropletEnvironmental scienceDiffusion (business)businessPhysics::Atmospheric and Oceanic PhysicsWater vapor0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
researchProduct

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
researchProduct

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
researchProduct

Influence of Saharan dust on cloud glaciation in southern Morocco during the Saharan Mineral Dust Experiment

2008

[1] Multiwavelength lidar, Sun photometer, and radiosonde observations were conducted at Ouarzazate (30.9°N, 6.9°W, 1133 m above sea level, asl), Morocco, in the framework of the Saharan Mineral Dust Experiment (SAMUM) in May–June 2006. The field site is close to the Saharan desert. Information on the depolarization ratio, backscatter and extinction coefficients, and lidar ratio of the dust particles, estimates of the available concentration of atmospheric ice nuclei at cloud level, profiles of temperature, humidity, and the horizontal wind vector as well as backward trajectory analysis are used to study cases of cloud formation in the dust with focus on heterogeneous ice formation. Surpris…

Atmospheric ScienceVirgaEcologyIce crystalsCloud topCloud seedingPaleontologySoil ScienceForestryAquatic ScienceMineral dustOceanographyAtmospheric sciencesGeophysicsSpace and Planetary ScienceGeochemistry and PetrologySea ice thicknessEarth and Planetary Sciences (miscellaneous)Ice nucleusEnvironmental scienceWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
researchProduct

Aerosol responses to precipitation along North American air trajectories arriving at Bermuda

2021

North American pollution outflow is ubiquitous over the western North Atlantic Ocean, especially in winter, making this location a suitable natural laboratory for investigating the impact of precipitation on aerosol particles along air mass trajectories. We take advantage of observational data collected at Bermuda to seasonally assess the sensitivity of aerosol mass concentrations and volume size distributions to accumulated precipitation along trajectories (APT). The mass concentration of particulate matter with aerodynamic diameter less than 2.5 µm normalized by the enhancement of carbon monoxide above background (PM2.5/ΔCO) at Bermuda was used to estimate the degree of aerosol loss durin…

Atmospheric Sciencecloud droplet number concentrationfood.ingredient010504 meteorology & atmospheric sciencesaerosolQC1-999010501 environmental sciencesAtmospheric sciences01 natural sciencesArticlefoodcloudMass concentration (chemistry)14. Life underwaterPrecipitationQD1-999ScavengingAir masslow clouds0105 earth and related environmental sciencesPhysicsSea saltParticulatesAerosolAERONETChemistry13. Climate actionEnvironmental scienceAtmospheric Chemistry and Physics
researchProduct

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
researchProduct