about
Ion-induced nucleation of pure biogenic particles.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.The formation of highly oxidized multifunctional products in the ozonolysis of cyclohexene.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.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-scale evidence of aerosol particle formation via sequential addition of HIO3.Production of neutral molecular clusters by controlled neutralization of mobility standards.The 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.Solar eclipse demonstrating the importance of photochemistry in new particle formation.Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere.A large source of low-volatility secondary organic aerosol.The role of ions in new particle formation in the CLOUD chamberExperimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperaturesGround-based observation of clusters and nucleation-mode particles in the AmazonDirect Observations of Atmospheric Aerosol NucleationDoes the onset of new particle formation occur in the planetary boundary layer?Measurements of cluster ions using a nano radial DMA and a particle size magnifier in CLOUDOn atmospheric neutral and ion clusters observed in Hyytiälä spring 2011The particle size magnifier closing the gap between measurement of molecules, molecular clusters and aerosol particlesHigh concentrations of sub-3nm clusters and frequent new particle formation observed in the Po Valley, Italy, during the PEGASOS 2012 campaignA new high-transmission inlet for the Caltech nano-RDMA for size distribution measurements of sub-3 nm ions at ambient concentrationsHeterogeneous Nucleation onto Ions and Neutralized Ions: Insights into Sign-PreferenceSulphuric acid and aerosol particle production in the vicinity of an oil refineryEvolution of alpha-pinene oxidation products in the presence of varying oxidizers: CI-APi-TOF point of viewIon-induced sulfuric acid–ammonia nucleation drives particle formation in coastal AntarcticaMulticomponent new particle formation from sulfuric acid, ammonia, and biogenic vaporsFormation and growth of sub-3-nm aerosol particles in experimental chambersHow well can we predict cluster fragmentation inside a mass spectrometer?Size-dependent influence of NOx on the growth rates of organic aerosol particles
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P50
description
hulumtues
@sq
researcher
@en
wetenschapper
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հետազոտող
@hy
name
Juha Kangasluoma
@ast
Juha Kangasluoma
@en
Juha Kangasluoma
@es
Juha Kangasluoma
@nl
Juha Kangasluoma
@sl
type
label
Juha Kangasluoma
@ast
Juha Kangasluoma
@en
Juha Kangasluoma
@es
Juha Kangasluoma
@nl
Juha Kangasluoma
@sl
prefLabel
Juha Kangasluoma
@ast
Juha Kangasluoma
@en
Juha Kangasluoma
@es
Juha Kangasluoma
@nl
Juha Kangasluoma
@sl
P106
P21
P31
P496
0000-0002-1639-1187