Elemental composition and clustering behaviour of α-pinene oxidation products for different oxidation conditionsEffect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass SpectrometryOxidation products of biogenic emissions contribute to nucleation of atmospheric particles.Ion-induced nucleation of pure biogenic particles.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.Real-time measurement of oligomeric species in secondary organic aerosol with the aerosol time-of-flight mass spectrometer.Insight into acid-base nucleation experiments by comparison of the chemical composition of positive, negative, and neutral clusters.Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation.Evidence for the role of organics in aerosol particle formation under atmospheric conditions.Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation.Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions.Global atmospheric particle formation from CERN CLOUD measurements.The effect of acid-base clustering and ions on the growth of atmospheric nano-particlesMolecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic moleculesThe role of low-volatility organic compounds in initial particle growth in the atmosphere.New particle formation in the free troposphere: A question of chemistry and timing.O/C and OM/OC ratios of primary, secondary, and ambient organic aerosols with high-resolution time-of-flight aerosol mass spectrometry.Combined determination of the chemical composition and of health effects of secondary organic aerosols: the POLYSOA project.Solar eclipse demonstrating the importance of photochemistry in new particle formation.Determination of the aerosol yield of isoprene in the presence of an organic seed with carbon isotope analysis.Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere.Using proton transfer reaction mass spectrometry for online analysis of secondary organic aerosols.Experimental investigation of ion–ion recombination under atmospheric conditionsCauses and importance of new particle formation in the present-day and preindustrial atmospheresInfluence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleationMeasurement–model comparison of stabilized Criegee intermediate and highly oxygenated molecule production in the CLOUD chamberNew particle formation in the sulfuric acid–dimethylamine–water system: reevaluation of CLOUD chamber measurements and comparison to an aerosol nucleation and growth modelEvaporation of sulfate aerosols at low relative humidityThe role of ions in new particle formation in the CLOUD chamberUnexpectedly acidic nanoparticles formed in dimethylamine–ammonia–sulfuric-acid nucleation experiments at CLOUDAqueous phase oxidation of sulphur dioxide by ozone in cloud dropletsEffect of ions on sulfuric acid-water binary particle formation: 2. Experimental data and comparison with QC-normalized classical nucleation theoryExperimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperaturesHeterogeneous ice nucleation of viscous secondary organic aerosol produced from ozonolysis of <i>α</i>-pineneHygroscopicity of nanoparticles produced from homogeneous nucleation in the CLOUD experimentsModeling the thermodynamics and kinetics of sulfuric acid-dimethylamine-water nanoparticle growth in the CLOUD chamberObservation of viscosity transition in <i>α</i>-pinene secondary organic aerosolPhase transition observations and discrimination of small cloud particles by light polarization in expansion chamber experimentsOn the composition of ammonia–sulfuric-acid ion clusters during aerosol particle formationThermodynamics of the formation of sulfuric acid dimers in the binary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O) and ternary (H<sub>2</sub>SO<sub>4</sub>–H<sub>2</sub>O–N
P50
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P50
description
French atmospheric researcher (University of Helsinki)
@en
natuurkundige
@nl
ranskalainen ilmakehäfyysikko ...... den tutkimuskeskuksessa (INAR)
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հետազոտող
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name
Jonathan Duplissy
@ast
Jonathan Duplissy
@de
Jonathan Duplissy
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Jonathan Duplissy
@es
Jonathan Duplissy
@fi
Jonathan Duplissy
@nl
Jonathan Duplissy
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Jonathan Duplissy
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type
label
Jonathan Duplissy
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Jonathan Duplissy
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Jonathan Duplissy
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Jonathan Duplissy
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Jonathan Duplissy
@fi
Jonathan Duplissy
@nl
Jonathan Duplissy
@sl
Jonathan Duplissy
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altLabel
Duplissy, J.
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prefLabel
Jonathan Duplissy
@ast
Jonathan Duplissy
@de
Jonathan Duplissy
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Jonathan Duplissy
@es
Jonathan Duplissy
@fi
Jonathan Duplissy
@nl
Jonathan Duplissy
@sl
Jonathan Duplissy
@sv
P227
P1053
A-1723-2010
P21
P227
1081537299
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P2930
J.Duplissy.2
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P3829
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0000-0001-8819-0264
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1980-02-21T00:00:00Z
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jonathan-duplissy