| human | Q5 |
| P227 | GND ID | 126106447X |
| P213 | ISNI | 0000000352740652 |
| P8980 | KANTO ID | 000142052 |
| P496 | ORCID iD | 0000-0002-0215-4893 |
| P3829 | Publons author ID | 2218752 |
| P1053 | ResearcherID | N-2571-2016 |
| P214 | VIAF ID | 1824166717390127150002 |
| P27 | country of citizenship | Finland | Q33 |
| P69 | educated at | University of Helsinki | Q28695 |
| P108 | employer | University of Helsinki | Q28695 |
| Ames Research Center | Q181052 | ||
| P734 | family name | Ehn | Q21510003 |
| Ehn | Q21510003 | ||
| Ehn | Q21510003 | ||
| P735 | given name | Mikael | Q15620350 |
| Mikael | Q15620350 | ||
| P106 | occupation | physicist | Q169470 |
| atmospheric scientist | Q17276189 | ||
| P39 | position held | associate professor | Q9344260 |
| P21 | sex or gender | male | Q6581097 |
| Q57864155 | A chamber study of the influence of boreal BVOC emissions and sulfuric acid on nanoparticle formation rates at ambient concentrations |
| Q21093466 | A high-resolution mass spectrometer to measure atmospheric ion composition |
| Q46927137 | A large source of low-volatility secondary organic aerosol |
| Q57531919 | A novel method for online analysis of gas and particle composition: description and evaluation of a Filter Inlet for Gases and AEROsols (FIGAERO) |
| Q57689567 | Aerosol hygroscopicity and CCN activation kinetics in a boreal forest environment during the 2007 EUCAARI campaign |
| Q58064959 | Aerosol properties associated with air masses arriving into the North East Atlantic during the 2008 Mace Head EUCAARI intensive observing period: an overview |
| Q57689573 | An Instrumental Comparison of Mobility and Mass Measurements of Atmospheric Small Ions |
| Q57689578 | Atmospheric ions and nucleation: a review of observations |
| Q60023202 | Atmospheric new particle formation from sulfuric acid and amines in a Chinese megacity |
| Q57689682 | Atmospheric nucleation: highlights of the EUCAARI project and future directions |
| Q115480192 | Atmospheric organic vapors in two European pine forests measured by a Vocus PTR-TOF: insights into monoterpene and sesquiterpene oxidation processes |
| Q57689445 | Atmospheric sulphuric acid and neutral cluster measurements using CI-APi-TOF |
| Q57689143 | Biogenic and biomass burning organic aerosol in a boreal forest at Hyytiälä, Finland, during HUMPPA-COPEC 2010 |
| Q91703737 | CI-Orbitrap: An Analytical Instrument To Study Atmospheric Reactive Organic Species |
| Q57689582 | Characterisation of corona-generated ions used in a Neutral cluster and Air Ion Spectrometer (NAIS) |
| Q57689761 | Characteristic features of air ions at Mace Head on the west coast of Ireland |
| Q58064896 | Characterization of organic compounds in 10- to 50-nm aerosol particles in boreal forest with laser desorption-ionization aerosol mass spectrometer and comparison with other techniques |
| Q48258961 | Chemical Characterization of Gas- and Particle-Phase Products from the Ozonolysis of α-Pinene in the Presence of Dimethylamine |
| Q38163595 | Chemistry of atmospheric nucleation: on the recent advances on precursor characterization and atmospheric cluster composition in connection with atmospheric new particle formation |
| Q37698363 | Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition |
| Q59309418 | Combined effects of boundary layer dynamics and atmospheric chemistry on aerosol composition during new particle formation periods |
| Q62774620 | Combined effects of boundary layer dynamics and atmospheric chemistry on aerosol composition during new particle formation periods |
| Q57689688 | Composition and temporal behavior of ambient ions in the boreal forest |
| Q47569364 | Computational Study of Hydrogen Shifts and Ring-Opening Mechanisms in α-Pinene Ozonolysis Products |
| Q57204064 | Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth |
| Q57689649 | Correction to “Relationship between aerosol oxidation level and hygroscopic properties of laboratory generated secondary organic aerosol (SOA) particles” |
| Q57689182 | Direct Observations of Atmospheric Aerosol Nucleation |
| Q58384403 | Direct measurement of NO3 radical reactivity in a boreal forest |
| Q114018838 | Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere |
| Q57689189 | Does the onset of new particle formation occur in the planetary boundary layer? |
| Q33464001 | Effects of chemical complexity on the autoxidation mechanisms of endocyclic alkene ozonolysis products: from methylcyclohexenes toward understanding α-pinene |
| Q114019086 | Eight years of sub-micrometre organic aerosol composition data from the boreal forest characterized using a machine-learning approach |
| Q21129046 | Elemental composition and clustering behaviour of α-pinene oxidation products for different oxidation conditions |
| Q58064669 | Estimating the contribution of organic acids to northern hemispheric continental organic aerosol |
| Q59707272 | Evidence for Diverse Biogeochemical Drivers of Boreal Forest New Particle Formation |
| Q57533242 | Evolution of Organic Aerosols in the Atmosphere |
| Q57689209 | Evolution of α-pinene oxidation products in the presence of varying oxidizers: Negative APi-TOF point of view |
| Q42082290 | Factors controlling the evaporation of secondary organic aerosol from α-pinene ozonolysis |
| Q40484079 | Formation of Highly Oxidized Radicals and Multifunctional Products from the Atmospheric Oxidation of Alkylbenzenes. |
| Q57866964 | Formation of highly oxidized multifunctional compounds: autoxidation of peroxy radicals formed in the ozonolysis of alkenes – deduced from structure–product relationships |
| Q57689492 | Gas phase formation of extremely oxidized pinene reaction products in chamber and ambient air |
| Q57689699 | Growth rates during coastal and marine new particle formation in western Ireland |
| Q64104145 | Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol |
| Q91719227 | How well can we predict cluster fragmentation inside a mass spectrometer? |
| Q37486956 | Hydroxyl radical-induced formation of highly oxidized organic compounds. |
| Q58064993 | Hygroscopicity and chemical composition of Antarctic sub-micrometre aerosol particles and observations of new particle formation |
| Q48043630 | Impact on short-lived climate forcers increases projected warming due to deforestation. |
| Q59807094 | In situ submicron organic aerosol characterization at a boreal forest research station during HUMPPA-COPEC 2010 using soft and hard ionization mass spectrometry |
| Q114109423 | Influence of biogenic emissions from boreal forests on aerosol–cloud interactions |
| Q58065068 | Iodine dioxide nucleation simulations in coastal and remote marine environments |
| Q116907748 | Isomer-Resolved Mobility-Mass Analysis of α-Pinene Ozonolysis Products |
| Q57263921 | Long-term cloud condensation nuclei number concentration, particle number size distribution and chemical composition measurements at regionally representative observatories |
| Q47196996 | Long-term observations of the background aerosol at Cabauw, The Netherlands |
| Q57689514 | Long-term volatility measurements of submicron atmospheric aerosol in Hyytiälä, Finland |
| Q56944480 | Measurement–model comparison of stabilized Criegee intermediate and highly oxygenated molecule production in the CLOUD chamber |
| Q57689288 | Measuring composition and growth of ion clusters of sulfuric acid, ammonia, amines and oxidized organics as first steps of nucleation in the CLOUD experiment |
| Q33465156 | Modeling the Charging of Highly Oxidized Cyclohexene Ozonolysis Products Using Nitrate-Based Chemical Ionization |
| Q57882474 | Modeling the role of highly oxidized multifunctional organic molecules for the growth of new particles over the boreal forest region |
| Q57863601 | Modelling the contribution of biogenic volatile organic compounds to new particle formation in the Jülich plant atmosphere chamber |
| Q37256141 | Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules |
| Q59750830 | Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors |
| Q58064868 | New insights into nocturnal nucleation |
| Q58064874 | Nitrogenated and aliphatic organic vapors as possible drivers for marine secondary organic aerosol growth |
| Q57689628 | Observations of Nano-CN in the Nocturnal Boreal Forest |
| Q33859278 | Observations of aminium salts in atmospheric nanoparticles and possible climatic implications |
| Q56944599 | On the composition of ammonia–sulfuric-acid ion clusters during aerosol particle formation |
| Q57689338 | Online atmospheric pressure chemical ionization ion trap mass spectrometry (APCI-IT-MSn) for measuring organic acids in concentrated bulk aerosol – a laboratory and field study |
| Q111897291 | Orbitool: a software tool for analyzing online Orbitrap mass spectrometry data |
| Q57689090 | Organic aerosol components derived from 25 AMS data sets across Europe using a consistent ME-2 based source apportionment approach |
| Q57689633 | Organic condensation: a vital link connecting aerosol formation to cloud condensation nuclei (CCN) concentrations |
| Q57867567 | Phase partitioning and volatility of secondary organic aerosol components formed from α-pinene ozonolysis and OH oxidation: the importance of accretion products and other low volatility compounds |
| Q91850960 | Primary Formation of Highly Oxidized Multifunctional Products in the OH-Initiated Oxidation of Isoprene: A Combined Theoretical and Experimental Study |
| Q35740454 | Production of extremely low volatile organic compounds from biogenic emissions: Measured yields and atmospheric implications |
| Q114603145 | Pyruvic acid in the boreal forest: gas-phase mixing ratios and impact on radical chemistry |
| Q57689643 | Quantification of the volatility of secondary organic compounds in ultrafine particles during nucleation events |
| Q42697871 | Rapid autoxidation forms highly oxidized RO2 radicals in the atmosphere |
| Q57689114 | Reactivity of stabilized Criegee intermediates (sCIs) from isoprene and monoterpene ozonolysis toward SO2 and organic acids |
| Q58064655 | Real-Time Detection of Arsenic Cations from Ambient Air in Boreal Forest and Lake Environments |
| Q57867467 | Relating the hygroscopic properties of submicron aerosol to both gas- and particle-phase chemical composition in a boreal forest environment |
| Q57689727 | Relationship between aerosol oxidation level and hygroscopic properties of laboratory generated secondary organic aerosol (SOA) particles |
| Q57881438 | Resolving anthropogenic aerosol pollution types – deconvolution and exploratory classification of pollution events |
| Q57251968 | Results and recommendations from an intercomparison of six Hygroscopicity-TDMA systems |
| Q34210669 | Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation |
| Q57689657 | Seasonal variation of CCN concentrations and aerosol activation properties in boreal forest |
| Q114110307 | Significance of the organic aerosol driven climate feedback in the boreal area |
| Q96231421 | Size-dependent influence of NOx on the growth rates of organic aerosol particles |
| Q57689120 | Sub-3 nm particle size and composition dependent response of a nano-CPC battery |
| Q61935648 | Suppression of new particle formation from monoterpene oxidation by NOx |
| Q114107358 | Terpene emissions from boreal wetlands can initiate stronger atmospheric new particle formation than boreal forests |
| Q57689668 | The effect of H 2 SO 4 – amine clustering on chemical ionization mass spectrometry (CIMS) measurements of gas-phase sulfuric acid |
| Q33463067 | The formation of highly oxidized multifunctional products in the ozonolysis of cyclohexene. |
| Q90287888 | The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system |
| Q56944527 | The role of ions in new particle formation in the CLOUD chamber |
| Q114543067 | Zeppelin-led study on the onset of new particle formation in the planetary boundary layer |
| Q51390529 | α-Pinene Autoxidation Products May Not Have Extremely Low Saturation Vapor Pressures Despite High O:C Ratios. |
| Mikael Ehn | wikipedia |
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