0000000000385879

AUTHOR

Frank Arnold

showing 6 related works from this author

The role of VOC oxidation products in continental new particle formation

2008

Abstract. Aerosol physical and chemical properties and trace gas concentrations were measured during the QUEST field campaign in March–April, 2003, in Hyytiälä, Finland. Our aim was to understand the role of oxidation products of VOC's such as mono- and sesquiterpenes in atmospheric nucleation events. Particle chemical compositions were measured using the Aerodyne Aerosol Mass Spectrometer, and chemical compositions of aerosol samples collected with low-pressure impactors and a high volume sampler were analysed using a number of techniques. The results indicate that during and after new particle formation, all particles larger than 50 nm in diameter contained similar organic substances that…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesChemistry[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereNucleationAnalytical chemistry010501 environmental sciencesMass spectrometry01 natural scienceslcsh:QC1-999Trace gasAerosollcsh:Chemistrylcsh:QD1-999Volume (thermodynamics)13. Climate actionDifferential mobility analyzerParticle/dk/atira/pure/subjectarea/asjc/1900/1902lcsh:Physics0105 earth and related environmental sciences
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Aerosol layers from the 2008 eruptions of Mount Okmok and Mount Kasatochi: In situ upper troposphere and lower stratosphere measurements of sulfate a…

2010

In 2008 Mount Okmok and Mount Kasatochi started erupting on 12 July and 7 August, respectively, in the Aleutians, depositing emissions of trace gases and aerosols as high as 15.2 km into the atmosphere. During an aircraft campaign, conducted over Europe in between 27 October and 2 November 2008, the volcanic aerosol was measured by an Aerodyne aerosol mass spectrometer, capable of particle chemical composition measurements covering a size diameter range between 40 nm and 1 mm. In the volcanic aerosol layer enhanced submicron particulate sulfate concentrations of up to 2.0 mg m−3 standard temperature and pressure (STP) were observed between 8 and 12 km altitude, while background values …

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesKasatochiSoil ScienceAerosol mass spectrometry010501 environmental sciencesAquatic ScienceOceanographyAtmospheric sciences01 natural sciencesTropospherechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyEarth and Planetary Sciences (miscellaneous)Volcanic aerosolSulfate aerosolSulfateStratosphere0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]EcologyAtmosphärische SpurenstoffePaleontologyForestryParticulatesTrace gasAerosolGeophysicschemistry13. Climate actionSpace and Planetary ScienceAirborne aerosol measurementsAerosol mass spectrometryvolcanic aerosol volcanic aerosolJournal of Geophysical Research
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In-situ observations of young contrails – overview and selected results from the CONCERT campaign

2010

Lineshaped contrails were detected with the research aircraft Falcon during the CONCERT – CONtrail and Cirrus ExpeRimenT – campaign in October/November 2008. The Falcon was equipped with a set of instruments to measure the particle size distribution, shape, extinction and chemical composition as well as trace gas mixing ratios of sulfur dioxide (SO<sub>2</sub>), reactive nitrogen and halogen species (NO, NO<sub>y</sub>, HNO<sub>3</sub>, HONO, HCl), ozone (O<sub>3</sub>) and carbon monoxide (CO). During 12 mission flights over Europe, numerous contrails, cirrus clouds and a volcanic aerosol layer were probed at altitudes between 8.5 and 11.6 km…

Atmospheric ScienceOzoneMeteorologyicecirrusSO2medicine.disease_causeAtmospheric scienceslcsh:Chemistrychemistry.chemical_compoundAltitudetrace gasesddc:550medicineLife ScienceFlugabteilung OberpfaffenhofenStratosphereIce crystalsInstitut für AntriebstechnikAtmosphärische SpurenstoffecontrailSootlcsh:QC1-999JTrace gaschemistrylcsh:QD1-999Extinction (optical mineralogy)Cirruslcsh:PhysicsAtmospheric Chemistry and Physics
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Telomerase and pluripotency factors jointly regulate stemness in pancreatic cancer stem cells

2021

© 2021 by the authors.

0301 basic medicineHomeobox protein NANOGCancer ResearchTelomerasePancreatic neoplasmsMedicinaBiologyStammzelleArticle03 medical and health sciences0302 clinical medicineSOX2Cancer stem cellPancreatic cancermedicineddc:610BauchspeicheldrüsenkrebsStemnessTelomeraseRC254-282Telomere lengthPancreas; CancerCancer stem cellsNeoplastic stem cellsCancer stem cells; Pancreatic cancer; Self-renewal; Stemness; Telomerase; Telomere lengthNeoplasms. Tumors. Oncology. Including cancer and carcinogensPancreatic cancermedicine.disease3. Good healthTelomere030104 developmental biologyOncologyKLF4030220 oncology & carcinogenesisCancer researchSelf-renewalStem cellDDC 610 / Medicine & health
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Measurements of HONO, NO, NOyand SO2in aircraft exhaust plumes at cruise

2011

Measurements of gaseous nitrogen and sulfur oxide emissions in young aircraft exhaust plumes give insight into chemical oxidation processes inside aircraft engines. Particularly, the OHA¢Â�Â�induced formation of nitrous acid (HONO) from nitrogen oxide (NO) and sulfuric acid (H2SO4) from sulfur dioxide (SO2) inside the turbine which is highly uncertain, need detailed analysis to address the climate impact of aviation. We report on airborne in situ measurements at cruise altitudes of HONO, NO, NOy, and SO2 in 9 wakes of 8 different types of modern jet airliners, including for the first time also an A380. Measurements of HONO and SO2 were made with an ITCIMS (Ion Trap Chemical Ionization Mass …

Chemical ionizationNitrous acidMeteorologychemistry.chemical_elementSulfuric acidAtmospheric sciencesSulfurSulfur oxidechemistry.chemical_compoundGeophysicschemistryGeneral Earth and Planetary SciencesEnvironmental scienceNitrogen oxideSulfur dioxideNOxGeophysical Research Letters
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HNO3 partitioning in cirrus clouds

1999

During the 1997 POLSTAR-1 winter campaign in northern Sweden a flight was performed across a cold trough of air (similar or equal to 196 K) in the tropopause region. Measurements of total water vapour, nitric acid, particles and reactive nitrogen (NOy) were taken. The particle measurements indicate that about 3% of the particles in the moist tropospheric air were ice particles. Forward and backward facing NOy inlets were used simultaneously to determine condensed phase HNO3. The combined NOy and particle measurements reveal that less than 1% of a monolayer of NOy could have resided on the ice particles. This casts doubt on the hypothesis that sedimenting cirrus particles generally lead to a…

Ice cloudReactive nitrogenAtmospheric sciencesJTropospherechemistry.chemical_compoundGeophysicschemistryNitric acidddc:550General Earth and Planetary SciencesEnvironmental scienceCirrusNitrogen oxideTropopauseWater vapor
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