Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors
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I. Riipinen | L. Ahonen | T. Petäjä | P. Winkler | A. Virtanen | R. Volkamer | D. Worsnop | R. Flagan | B. Baumgartner | J. Kirkby | W. Nie | M. Kulmala | C. Hoyle | U. Baltensperger | K. Carslaw | M. Rissanen | T. Nieminen | V. Kerminen | A. Onnela | S. Schuchmann | A. Hansel | D. Wimmer | L. Dada | J. Tröstl | J. Dommen | P. Ye | M. Ehn | M. Passananti | M. Sipilä | H. Gordon | N. Donahue | Chao Yan | S. Schallhart | Xuemeng Chen | K. Lehtipalo | J. Curtius | D. Draper | C. Rose | J. Kangasluoma | M. Breitenlechner | R. Wagner | R. Mauldin | L. Heikkinen | Changhyuk Kim | A. Buchholz | S. Mathot | J. Duplissy | Q. Zha | Mingyi Wang | O. Väisänen | N. Sarnela | T. Jokinen | J. Hakala | V. Pospisilova | O. Garmash | A. Dias | F. Piel | F. Bianchi | J. Kontkanen | M. Xiao | L. Quéléver | L. Fischer | Johanna Helm | L. Nichman | A. Kürten | C. Tauber | A. Baccarini | A. Tomé | A. Vogel | C. Fuchs | M. Heinritzi | M. Simon | A. Wagner | C. Frege | K. Sengupta | Dexian Chen | A. Amorim | S. Brilke | P. Bauer | V. Hofbauer | Xucheng He | H. Finkenzeller | D. Stolzenburg | U. Molteni | A. Bergen | H. Mai | A. Ojdanic | Anne-Kathrin Bernhammer | A. Ylisirniö | M. Lawler | L. Weitz | S. Mazon | Federico Bianchi | Henning Finkenzeller | A. Wagner
[1] T. Petäjä,et al. The role of highly oxygenated molecules (HOMs) in determining the composition of ambient ions in the boreal forest , 2017 .
[2] A. Hansel,et al. PTR3: An Instrument for Studying the Lifecycle of Reactive Organic Carbon in the Atmosphere. , 2017, Analytical chemistry.
[3] Mindong Chen,et al. Laboratory observations of temperature and humidity dependencies of nucleation and growth rates of sub‐3 nm particles , 2017 .
[4] P. Winkler,et al. submitter : A DMA-train for precision measurement of sub-10 nm aerosol dynamics , 2016 .
[5] G. Mann,et al. Global atmospheric particle formation from CERN CLOUD measurements , 2016, Science.
[6] T. Petäjä,et al. Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures , 2016 .
[7] J. Curtius,et al. Observation of new particle formation and measurement of sulfuric acid,ammonia, amines and highly oxidized organic molecules at a rural site incentral Germany , 2016 .
[8] D. Ceburnis,et al. Molecular scale evidence of new particle formation via sequential addition of HIO3 , 2016, Nature.
[9] T. Petäjä,et al. New particle formation in the free troposphere: A question of chemistry and timing , 2016, Science.
[10] J. Seinfeld,et al. Ion-induced nucleation of pure biogenic particles , 2016, Nature.
[11] I. Riipinen,et al. The role of low-volatility organic compounds in initial particle growth in the atmosphere , 2016, Nature.
[12] Olli-Pekka Tikkanen,et al. Analysis of sub-3 nm particle growth in connection with sulfuric acid in a boreal forest , 2016 .
[13] T. Petäjä,et al. On the accuracy of ion measurements using a neutral cluster and air ion spectrometer , 2016 .
[14] João Almeida,et al. The effect of acid–base clustering and ions on the growth of atmospheric nano-particles , 2016, Nature Communications.
[15] K. Lehtinen,et al. Growth of atmospheric clusters involving cluster–cluster collisions: comparison of different growth rate methods , 2016 .
[16] T. Petäjä,et al. Heterogeneous Nucleation onto Ions and Neutralized Ions: Insights into Sign-Preference , 2016 .
[17] D. Brus,et al. Effect of ions on sulfuric acid‐water binary particle formation: 2. Experimental data and comparison with QC‐normalized classical nucleation theory , 2016 .
[18] A. Hansel,et al. Characterization of the mass-dependent transmission efficiency of a CIMS , 2015 .
[19] I. Riipinen,et al. Growth rates of atmospheric molecular clusters based on appearance times and collision-evaporation fluxes : Growth by monomers , 2014 .
[20] João Almeida,et al. Neutral molecular cluster formation of sulfuric acid–dimethylamine observed in real time under atmospheric conditions , 2014, Proceedings of the National Academy of Sciences.
[21] J. Smith,et al. Secondary Organic Aerosol Formation and Organic Nitrate Yield from NO3 Oxidation of Biogenic Hydrocarbons , 2014, Environmental science & technology.
[22] T. Petäjä,et al. Methods for determining particle size distribution and growth rates between 1 and 3 nm using the Particle Size Magnifier , 2014 .
[23] D. R. Hanson,et al. Stabilization of sulfuric acid dimers by ammonia, methylamine, dimethylamine, and trimethylamine , 2014 .
[24] Keywan Riahi,et al. Air-pollution emission ranges consistent with the representative concentration pathways , 2014 .
[25] J. Seinfeld,et al. Oxidation Products of Biogenic Emissions Contribute to Nucleation of Atmospheric Particles , 2014, Science.
[26] H. Kjaergaard,et al. A large source of low-volatility secondary organic aerosol , 2014, Nature.
[27] Y. Rudich,et al. Suppression of new particle formation from monoterpene oxidation by NO x , 2013 .
[28] T. Petäjä,et al. Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules , 2013, Proceedings of the National Academy of Sciences.
[29] J. Seinfeld,et al. Molecular understanding of sulphuric acid–amine particle nucleation in the atmosphere , 2013, Nature.
[30] S. Haider,et al. Characterisation of organic contaminants in the CLOUD chamber at CERN , 2013 .
[31] A. Hamed,et al. Formation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparison , 2013 .
[32] I. Riipinen,et al. Direct Observations of Atmospheric Aerosol Nucleation , 2013, Science.
[33] Eero Nikinmaa,et al. Station for Measuring Ecosystem-Atmosphere Relations: SMEAR , 2013 .
[34] U. Baltensperger,et al. Dimethylamine and ammonia measurements with ion chromatography during the CLOUD4 campaign , 2012 .
[35] Douglas R. Worsnop,et al. The contribution of organics to atmospheric nanoparticle growth , 2012 .
[36] J. Smith,et al. Size and time-resolved growth rate measurements of 1 to 5 nm freshly formed atmospheric nuclei , 2012 .
[37] Min Hu,et al. Nucleation and growth of nanoparticles in the atmosphere. , 2012, Chemical reviews.
[38] R. McGraw,et al. Effects of amines on formation of sub‐3 nm particles and their subsequent growth , 2012 .
[39] A. Mirme,et al. The mathematical principles and design of the NAIS – a spectrometer for the measurement of cluster ion and nanometer aerosol size distributions , 2011 .
[40] T. Petäjä,et al. Atmospheric sulphuric acid and neutral cluster measurements using CI-APi-TOF , 2011 .
[41] D. R. Hanson,et al. Ambient pressure proton transfer mass spectrometry: detection of amines and ammonia. , 2011, Environmental science & technology.
[42] Jorge Lima,et al. Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation , 2011, Nature.
[43] T. Petäjä,et al. Particle Size Magnifier for Nano-CN Detection , 2011 .
[44] J. Curtius,et al. Performance of a corona ion source for measurement of sulfuric acid by chemical ionization mass spectrometry , 2010 .
[45] K. Lehtinen,et al. Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed , 2010 .
[46] A. Arneth,et al. EUCAARI ion spectrometer measurements at 12 European sites – analysis of new particle formation events , 2010 .
[47] U. Rohner,et al. A high-resolution mass spectrometer to measure atmospheric ion composition , 2010 .
[48] John H. Seinfeld,et al. Effect of NO x level on secondary organic aerosol (SOA) formation from the photooxidation of terpenes , 2007 .
[49] G. Mann,et al. The contribution of boundary layer nucleation events to total particle concentrations on regional and global scales , 2006 .
[50] Frank Arnold,et al. Atmospheric sulphuric acid and aerosol formation : implications from atmospheric measurements for nucleation and early growth mechanisms , 2006 .
[51] Albert A Presto,et al. Secondary organic aerosol production from terpene ozonolysis. 2. Effect of NOx concentration. , 2005, Environmental science & technology.
[52] M. Pihlatie,et al. Sulphuric acid closure and contribution to nucleation mode particle growth , 2004 .
[53] Edward Charles Fortner,et al. Atmospheric New Particle Formation Enhanced by Organic Acids , 2004, Science.
[54] Tuomas Laurila,et al. Canopy scale monoterpene emissions of Pinus sylvestris dominated forests , 2000 .
[55] P. Mcmurry,et al. MEASURED ATMOSPHERIC NEW PARTICLE FORMATION RATES: IMPLICATIONS FOR NUCLEATION MECHANISMS , 1996 .
[56] D. Tanner,et al. Measurement of the gas phase concentration of H2SO4 and methane sulfonic acid and estimates of H2SO4 production and loss in the atmosphere , 1993 .
[57] Agnieszka,et al. The effect of acid-base clustering and ions on the growth of atmospheric nanoparticles , 2022 .