scholarly article | Q13442814 |
P819 | ADS bibcode | 2016JGRD..121.1752D |
P356 | DOI | 10.1002/2015JD023539 |
P50 | author | Jasper Kirkby | Q6163986 |
Markku Kulmala | Q11881063 | ||
Ken Carslaw | Q23769960 | ||
Juha Kangasluoma | Q37382780 | ||
Joachim Curtius | Q37382809 | ||
Katrianne Lehtipalo | Q37382858 | ||
Armin Hansel | Q37382884 | ||
Heikki Junninen | Q37382914 | ||
Antonio Amorim | Q38230454 | ||
Tuukka Petäjä | Q42304750 | ||
Siegfried Schobesberger | Q42841124 | ||
Neil M. Donahue | Q42881849 | ||
Jonathan Duplissy | Q43274823 | ||
Douglas Worsnop | Q29860697 | ||
Gerhard Steiner | Q37382518 | ||
Andreas Kürten | Q37382678 | ||
Federico Bianchi | Q37382728 | ||
Eimear Maria Dunne | Q43829605 | ||
Henning Henschel | Q43829624 | ||
David Brus | Q55507393 | ||
Mikko Sipilä | Q56425254 | ||
Vladimir Makhmutov | Q56427544 | ||
Tuomo Nieminen | Q56440736 | ||
Anni E. Määttänen | Q56451499 | ||
Josef Dommen | Q58180506 | ||
Daniela Wimmer | Q58180635 | ||
Agnieszka Kupc | Q60617034 | ||
Urs Baltensperger | Q83676007 | ||
P2093 | author name string | A. Onnela | |
R. Guida | |||
J. Merikanto | |||
J. Almeida | |||
A. Franchin | |||
F. Riccobono | |||
G. Tsagkogeorgas | |||
L. Rondo | |||
P. E. Wagner | |||
S. Mathot | |||
A. P. Praplan | |||
A. Tome | |||
A. Vrtala | |||
F. Stratmann | |||
H. Vehkamäki | |||
H. Vuollekoski | |||
H. Walther | |||
M. Breitenlechner | |||
P. Barmet | |||
R. C. Flagan | |||
P2860 | cites work | A high-resolution mass spectrometer to measure atmospheric ion composition | Q21093466 |
Calibration of a chemical ionization mass spectrometer for the measurement of gaseous sulfuric acid | Q39648251 | ||
Relation between electrical mobility, mass, and size for nanodrops 1-6.5 nm in diameter in air | Q23910452 | ||
Experimental evidence for the role of ions in particle nucleation under atmospheric conditions | Q29394105 | ||
Oxidation products of biogenic emissions contribute to nucleation of atmospheric particles | Q30821881 | ||
Insight into acid-base nucleation experiments by comparison of the chemical composition of positive, negative, and neutral clusters | Q33463377 | ||
Evidence for the role of organics in aerosol particle formation under atmospheric conditions. | Q33859238 | ||
Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation | Q34210669 | ||
Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions | Q34409197 | ||
Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules | Q37256141 | ||
Formation of nanoparticles of blue haze enhanced by anthropogenic pollution | Q37379765 | ||
Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere | Q43829556 | ||
A large source of low-volatility secondary organic aerosol | Q46927137 | ||
Atmospheric new particle formation enhanced by organic acids | Q47336479 | ||
Experimental investigation of ion–ion recombination under atmospheric conditions | Q55090434 | ||
Review of the vapour pressures of ice and supercooled water for atmospheric applications | Q55868926 | ||
SOLAR INFLUENCES ON CLIMATE | Q56482847 | ||
Cosmic Rays and Climate | Q56489833 | ||
On the derivation of particle nucleation rates from experimental formation rates | Q56944591 | ||
On the composition of ammonia–sulfuric-acid ion clusters during aerosol particle formation | Q56944599 | ||
Characterisation of organic contaminants in the CLOUD chamber at CERN | Q56944609 | ||
A fibre-optic UV system for H2SO4 production in aerosol chambers causing minimal thermal effects | Q56944687 | ||
Results from the CERN pilot CLOUD experiment | Q56944710 | ||
Performance of diethylene glycol-based particle counters in the sub-3 nm size range | Q57204059 | ||
Numerical simulations of mixing conditions and aerosol dynamics in the CERN CLOUD chamber | Q57204063 | ||
Contribution of sulfuric acid and oxidized organic compounds to particle formation and growth | Q57204064 | ||
Performance of a corona ion source for measurement of sulfuric acid by chemical ionization mass spectrometry | Q57204068 | ||
The use of the pulse height analyser ultrafine condensation particle counter (PHA-UCPC) technique applied to sizing of nucleation mode particles of differing chemical composition | Q57252011 | ||
Nucleation and Growth of Nanoparticles in the Atmosphere | Q57270387 | ||
Enhancement of atmospheric H2SO4 / H2O nucleation: organic oxidation products versus amines | Q57689038 | ||
Direct Observations of Atmospheric Aerosol Nucleation | Q57689182 | ||
Remarks on Ion Generation for CPC Detection Efficiency Studies in Sub-3-nm Size Range | Q57689367 | ||
Atmospheric sulphuric acid and neutral cluster measurements using CI-APi-TOF | Q57689445 | ||
Homogenous nucleation of sulfuric acid and water at close to atmospherically relevant conditions | Q57689614 | ||
Particle Size Magnifier for Nano-CN Detection | Q57689637 | ||
Composition and temporal behavior of ambient ions in the boreal forest | Q57689688 | ||
EUCAARI ion spectrometer measurements at 12 European sites – analysis of new particle formation events | Q57689692 | ||
The Role of Sulfuric Acid in Atmospheric Nucleation | Q57689738 | ||
Formation and growth rates of ultrafine atmospheric particles: a review of observations | Q57689802 | ||
Laboratory-measured nucleation rates of sulfuric acid and water binary homogeneous nucleation from the SO2+ OH reaction | Q57732007 | ||
Technical Note: Using DEG-CPCs at upper tropospheric temperatures | Q57891915 | ||
Effect of ions on sulfuric acid-water binary particle formation: 1. Theory for kinetic- and nucleation-type particle formation and atmospheric implications | Q58064631 | ||
Sub-10 nm particle growth by vapor condensation – effects of vapor molecule size and particle thermal speed | Q58065020 | ||
Rapid Formation of Sulfuric Acid Particles at Near-Atmospheric Conditions | Q58065307 | ||
An improved model for hydrate formation in sulfuric acid–water nucleation | Q58065409 | ||
An improved parameterization for sulfuric acid–water nucleation rates for tropospheric and stratospheric conditions | Q58065411 | ||
Analysis of the growth of nucleation mode particles observed in Boreal forest | Q58065521 | ||
Experiments on gas–liquid nucleation of sulfuric acid and water | Q58065562 | ||
Binary heterogeneous nucleation of a water-sulphuric acid system: The effect of hydrate interaction | Q58065665 | ||
Extended hydrates interaction model: Hydrate formation and the energetics of binary homogeneous nucleation | Q58065667 | ||
Binary nucleation of water–sulfuric acid system: Comparison of classical theories with different H2SO4 saturation vapor pressures | Q58065676 | ||
Impact of nucleation on global CCN | Q58072087 | ||
An Ultrafine Aerosol Condensation Nucleus Counter | Q58094488 | ||
Experimental Measurement of Competitive Ion-Induced and Binary Homogeneous Nucleation in SO2/H2O/N2Mixtures | Q58294748 | ||
Effect of Working Fluid on Sub-2 nm Particle Detection with a Laminar Flow Ultrafine Condensation Particle Counter | Q58295799 | ||
Gaseous ammonia and ammonium ions in the free troposphere | Q59064049 | ||
P433 | issue | 4 | |
P304 | page(s) | 1752-1775 | |
P577 | publication date | 2016-02-16 | |
P1433 | published in | Journal of Geophysical Research: Atmospheres | Q27724309 |
P1476 | title | Effect of ions on sulfuric acid-water binary particle formation: 2. Experimental data and comparison with QC-normalized classical nucleation theory | |
P478 | volume | 121 |
Q56627327 | Causes and importance of new particle formation in the present-day and preindustrial atmospheres |
Q33469905 | Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation |
Q28829189 | Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass Spectrometry |
Q58064631 | Effect of ions on sulfuric acid-water binary particle formation: 1. Theory for kinetic- and nucleation-type particle formation and atmospheric implications |
Q56944552 | Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures |
Q89687025 | Formation and growth of sub-3-nm aerosol particles in experimental chambers |
Q58416057 | Impacts of Cosmic Dust on Planetary Atmospheres and Surfaces |
Q57885017 | Intercomparison study and optical asphericity measurements of small ice particles in the CERN CLOUD experiment |
Q58058794 | Isoprene suppression of new particle formation: Potential mechanisms and implications |
Q57882318 | Long-term analysis of clear-sky new particle formation events and nonevents in Hyytiälä |
Q56944572 | Modeling the thermodynamics and kinetics of sulfuric acid-dimethylamine-water nanoparticle growth in the CLOUD chamber |
Q58181428 | Molecular-resolution simulations of new particle formation: Evaluation of common assumptions made in describing nucleation in aerosol dynamics models |
Q47806290 | Overview: Homogeneous nucleation from the vapor phase-The experimental science |
Q57882230 | Technical note: Conversion of isoprene hydroxy hydroperoxides (ISOPOOHs) on metal environmental simulation chamber walls |
Q36925572 | The effect of acid-base clustering and ions on the growth of atmospheric nano-particles |
Q56944527 | The role of ions in new particle formation in the CLOUD chamber |
Q39137666 | The role of low-volatility organic compounds in initial particle growth in the atmosphere. |
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