Search results for "Atmospheric chemistry"

showing 10 items of 93 documents

Evaluation of the global aerosol model EMAC-MADE3 in the uncoupled version - 12 h data

2018

Project: EMAC-MADE3 uncoupled - Recently, the aerosol microphysics submodel MADE3 was introduced as a successor to MADE and MADE-in. It includes nine aerosol species and nine lognormal modes to represent aerosol particles of three different mixing states throughout the aeroso size spectrum. Here we describe the implementation of the most recent version of MADE3 into the atmospheric chemistry general circulation model EMAC, including a detailed evaluation of a ten-year aerosol simulation with MADE3 as part of EMAC. Summary: Simulation with most recent version of MADE3 into the atmospheric chemistry general circulation model EMAC, including a detailed evaluation of a ten-year aerosol simulati…

atmospheric chemistryaerosolClimateEMAC-MADE3_uncoupled
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Chemie von Aerosolen

2007

Atmospharische Aerosolpartikel sind keine chemisch inerten Teilchen, deren Bildungsmechanismen, Verweildauer oder Funktion in der Atmosphare lediglich von mechanischen oder physikalischen Prozessen abhangen. Sowohl bei der Bildung von Aerosolpartikeln als auch im Verlauf ihres Verbleibs in der Atmosphare spielen chemische Reaktionen eine wesentliche Rolle. Chemische Reaktionen laufen an der Oberflache und im Inneren von Aerosolpartikeln ab und konnen sowohl die atmospharische Gasphasenchemie beeinflussen, z.B. indem sie sowohl als Reaktionsmedium fur ansonsten langsam verlaufende Gasphasenreaktionen dienen, als auch die Eigenschaften der Partikel, beispielsweise ihre Funktion als Kondensati…

atmospheric chemistryparticleChemistryPolymer chemistryCloud condensation nucleiPhysical chemistryaerosol - chemistryGeneral ChemistrySoot particlesChemical reactionGas phaseAerosolChemie in unserer Zeit
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New tracer compounds for secondary organic aerosol formation from β-caryophyllene oxidation

2013

Abstract Five products from β-caryophyllene oxidation (β-caryophyllonic acid (I), 3,3-dimethyl-2-(3-oxobutyl)cyclobutanecarboxylic acid (βCA198) (II), β-nocaryophyllonic acid (III), β-caryophyllinic acid (IV), and 2-(2-carboxyethyl)-3,3-dimethylcyclobutanecarboxylic acid (βCA200) (V)) were synthesized and their structures confirmed by nuclear magnetic resonance spectroscopy. Reaction chamber experiments with β-caryophyllene at two different ozone mixing ratios were performed and the carboxylic acid oxidation products in the particle phase were characterized by APCI–MS and HPLC–ESI–MS. All five synthesized acids were found as β-caryophyllene oxidation products in the reaction chamber aerosol…

chemistry.chemical_classificationAtmospheric ScienceOzonolysisOzoneCarboxylic acidInorganic chemistryNuclear magnetic resonance spectroscopySesquiterpeneAerosolchemistry.chemical_compoundchemistryAtmospheric chemistryTRACERGeneral Environmental ScienceAtmospheric Environment
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The Amazonian boundary layer and mesoscale circulations

2009

Numerous biogenic volatile organic compounds (VOC) species are released into the atmosphere from tropical forests. Measuring all those which are relevant for atmospheric chemistry or for the carbon budget is challenging. Large-Scale Biosphere-Atmosphere (LBA) Experiment field campaigns substantially increased the number of field studies of isoprene and monoterpene emissions, as well as of the exchange of several other VOC species. This chapter reports about the progress made within LBA from primary emission measurements at the plant species level up to discussions of the oxidative capacity of the atmosphere and formation of secondary organic aerosol particles and cloud condensation nuclei f…

chemistry.chemical_classificationHydrologyAmazonianchemistry.chemical_elementAerosolAtmospherechemistry.chemical_compoundchemistryEnvironmental chemistryAtmospheric chemistryCloud condensation nucleiEnvironmental scienceVolatile organic compoundCarbonIsoprene
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Emissions of atmospherically reactive gases nitrous acid and nitric oxide from Arctic permafrost peatlands

2022

Soils are important sources of nitric oxide (NO) and nitrous acid (HONO) in the atmosphere. These nitrogen (N)-containing gases play a crucial role in atmospheric chemistry and climate at different scales because of reactions modulated by NO and hydroxyl radicals (OH), which are formed via HONO photolysis. Northern permafrost soils have so far remained unexplored for HONO and NO emissions despite their high N stocks, capacity to emit nitrous oxide (N2O), and enhancing mineral N turnover due to warming and permafrost thawing. Here, we report the first HONO and NO emissions from high-latitude soils based on measurements of permafrost-affected subarctic peatlands. We show large HONO (0.1–2.4 µ…

denitrifikaatioatmospheric chemistrymaaperätyppioksidiarktinen aluesoil nitrogen cycledenitrificationnitrifikaatioHONO and NOnitrificationilmakemiaekosysteemit (ekologia)aineiden kiertopäästötArctic ecosystem
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Stratospheric aerosol-Observations, processes, and impact on climate

2016

Interest in stratospheric aerosol and its role in climate have increased over the last decade due to the observed increase in stratospheric aerosol since 2000 and the potential for changes in the sulfur cycle induced by climate change. This review provides an overview about the advances in stratospheric aerosol research since the last comprehensive assessment of stratospheric aerosol was published in 2006. A crucial development since 2006 is the substantial improvement in the agreement between in situ and space-based inferences of stratospheric aerosol properties during volcanically quiescent periods. Furthermore, new measurement systems and techniques, both in situ and space based, have be…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAir pollutionClimate changeSulfur cyclerespiratory system010502 geochemistry & geophysicsmedicine.disease_causeAtmospheric sciencescomplex mixtures01 natural sciencesAerosolchemistry.chemical_compoundGeophysicschemistryVolcano13. Climate actionAtmospheric chemistryClimatologymedicineEnvironmental scienceClimate model0105 earth and related environmental sciencesCarbonyl sulfideReviews of Geophysics
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2018

Volcanoes are a significant halogen source to the atmosphere. After water, carbon dioxide and sulfur compounds, halogens are often the most abundant gases in volcanic plumes. In the past, less attention was given to the heavy halogens bromine and iodine. However, the discovery of bromine monoxide (BrO) in volcanic plumes led to new interest especially in volcanic bromine chemistry and its impact on atmospheric processes. The BrO detection came along with advances in volcanic remote sensing techniques, in particular, robust DOAS applications and the possibility of continuous measurements by automated instruments located at safe distances from the volcano. As one of the consequences, the volc…

geographygeography.geographical_feature_categoryBromine010504 meteorology & atmospheric scienceschemistry.chemical_element010502 geochemistry & geophysicsAtmospheric sciences01 natural sciences7. Clean energyAerosolPlumeAtmosphereTroposphereVolcanochemistry13. Climate actionAtmospheric chemistryHalogenGeneral Earth and Planetary Sciences0105 earth and related environmental sciencesFrontiers in Earth Science
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Multicopter measurements of volcanic gas emissions at Masaya (Nicaragua), Turrialba (Costa Rica) and Stromboli (Italy) volcanoes: Applications for vo…

2017

Abstract. Volcanoes are a natural source of several reactive gases (e.g. sulfur and halogen containing species), as well as non-reactive gases (e.g. carbon dioxide). Besides that, halogen chemistry in volcanic plumes might have important impacts on atmospheric chemistry, carbon to sulfur ratios and sulfur dioxide fluxes are important established parameters to gain information on subsurface processes. In this study we demonstrate the successful deployment of a multirotor UAV (quadcopter) system with custom-made lightweight payloads on board for the compositional analysis and gas flux estimation of volcanic plumes. The various applications and their potential with such new measurement strateg…

geographygeography.geographical_feature_categoryDifferential optical absorption spectroscopyMineralogychemistry.chemical_elementSulfurPlumechemistry.chemical_compoundFlux (metallurgy)VolcanochemistryAtmospheric chemistryGas compositionGeologySulfur dioxide
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Volcanic CO2 flux measurement at Campi Flegrei by tunable diode laser absorption spectroscopy

2014

Near-infrared room-temperature Tunable Diode Lasers (TDL) have recently found increased usage in atmospheric chemistry and air monitoring research, but applications in volcanology are still limited to a few examples. Here, we explored the potential of a commercial infrared laser unit (GasFinder 2.0 from Boreal Laser Ltd) for measurement of volcanic CO2 mixing ratios, and ultimately for estimating the volcanic CO2 flux. Our field tests were conducted at Campi Flegrei near Pozzuoli, Southern Italy, where the GasFinder was used during three campaigns in October 2012, January 2013 and May 2013 to repeatedly measure the path-integrated mixing ratios of CO2 along cross-sections of the atmospheric…

geographygeography.geographical_feature_categoryTunable diode laser absorption spectroscopyVolcanic CO2 fluxesFar-infrared laserMineralogyVolcanologyLaser7. Clean energyFumaroleSettore GEO/08 - Geochimica E Vulcanologialaw.inventionTunable diode lasers Atmospheric CO2 monitoring Volcanic CO2 fluxes Campi FlegreiAtmosphereVolcanotunable diode lasers atmospheric CO2 monitoring volcanic gas sensing by laser spectroscopy volcanic CO2 fluxes Campi Flegrei13. Climate actionGeochemistry and PetrologylawAtmospheric chemistryAtmospheric CO2 monitoringTunable diode lasersCampi FlegreiGeologyRemote sensingBulletin of Volcanology
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Experimental FTIR-MI and Theoretical Studies of Isocyanic Acid Aggregates

2023

Homoaggregates of isocyanic acid (HNCO) were studied using FTIR spectroscopy combined with a low-temperature matrix isolation technique and quantum chemical calculations. Computationally, the structures of the HNCO dimers and trimers were optimized at the MP2, B3LYPD3 and B2PLYPD3 levels of theory employing the 6-311++G(3df,3pd) basis set. Topological analysis of the electron density (AIM) was used to identify the type of non-covalent interactions in the studied aggregates. Five stable minima were located on the potential energy surface for (HNCO)2, and nine were located on the potential energy surface for (HNCO)3. The most stable dimer (D1) involves a weak, almost linear N-H⋯N hydrog…

hydrogen bondatmospheric chemistryvetysidoksetOrganic ChemistryspektroskopiaPharmaceutical ScienceHNCOintermolecular interactionlaskennallinen kemiasolid argoncomputational chemistrymatrix isolation (MI)vibrational spectroscopyAnalytical Chemistryilmakemiamolecular complexChemistry (miscellaneous)Drug DiscoveryMolecular MedicinePhysical and Theoretical ChemistryFourier transform infrared (FTIR)Molecules
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