| Q56681030 | A General Theory of Climate Denial |
| Q56963237 | A cosmic ray-climate link and cloud observations |
| Q46242444 | A density functional theory study of aldehydes and their atmospheric products participating in nucleation |
| Q46927137 | A large source of low-volatility secondary organic aerosol |
| Q90448369 | A possible unaccounted source of atmospheric sulfate formation: amine-promoted hydrolysis and non-radical oxidation of sulfur dioxide |
| Q56158592 | A review of the relevance of the ‘CLOUD’ results and other recent observations to the possible effect of cosmic rays on the terrestrial climate |
| Q34578413 | A velocity map imaging photoelectron spectrometer for the study of ultrafine aerosols with a table-top VUV laser and Na-doping for particle sizing applied to dimethyl ether condensation. |
| Q52625837 | Accurate representations of the physicochemical properties of atmospheric aerosols: when are laboratory measurements of value? |
| Q52974016 | Accurate thermodynamic properties of gas phase hydrogen bonded complexes. |
| Q36414913 | Acid-base chemical reaction model for nucleation rates in the polluted atmospheric boundary layer |
| Q57948684 | Aerosols in the Pre-industrial Atmosphere |
| Q94671746 | Airborne particles might grow fast in cities |
| Q31138754 | Amazon boundary layer aerosol concentration sustained by vertical transport during rainfall |
| Q30488701 | Analytical Model for Estimating Terrestrial Cosmic Ray Fluxes Nearly Anytime and Anywhere in the World: Extension of PARMA/EXPACS. |
| Q91845660 | Assessment of the DLPNO Binding Energies of Strongly Noncovalent Bonded Atmospheric Molecular Clusters |
| Q48051233 | Atmospheric implication of the hydrogen bonding interaction in hydrated clusters of HONO and dimethylamine in the nighttime. |
| Q58103187 | Atmospheric nanoparticles and climate change |
| Q57264071 | Biogenic Potassium Salt Particles as Seeds for Secondary Organic Aerosol in the Amazon |
| Q93000557 | Bulk ultrafine grained/nanocrystalline metals via slow cooling |
| Q40439812 | Characteristics of ammonia gas and fine particulate ammonium from two distinct urban areas: Osaka, Japan, and Ho Chi Minh City, Vietnam |
| Q57881615 | Chemical characterization of atmospheric ions at the high altitude research station Jungfraujoch (Switzerland) |
| Q56083062 | Cloud formation may be linked to cosmic rays |
| Q50979451 | Communication: kinetics of scavenging of small, nucleating clusters: first nucleation theorem and sum rules. |
| Q33460982 | Comparing simulated and experimental molecular cluster distributions |
| Q33469905 | Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation |
| Q28595514 | Contribution of Arctic seabird-colony ammonia to atmospheric particles and cloud-albedo radiative effect |
| Q56627328 | Cosmic rays, aerosols, clouds, and climate: Recent findings from the CLOUD experiment |
| Q21994549 | Cosmic rays, solar activity and the climate |
| Q36480549 | Dimethylamine as a major alkyl amine species in particles and cloud water: Observations in semi-arid and coastal regions |
| Q35212496 | Dynamical evidence for causality between galactic cosmic rays and interannual variation in global temperature |
| Q21129060 | Earth's energy imbalance and implications |
| Q58244931 | Effect of Hydration and Base Contaminants on Sulfuric Acid Diffusion Measurement: A Computational Study |
| 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 |
| Q56944544 | Effect of ions on sulfuric acid-water binary particle formation: 2. Experimental data and comparison with QC-normalized classical nucleation theory |
| Q21129046 | Elemental composition and clustering behaviour of α-pinene oxidation products for different oxidation conditions |
| Q58054985 | Energetic Particle Influence on the Earth’s Atmosphere |
| Q55982548 | Evidence of nearby supernovae affecting life on Earth |
| Q56944552 | Experimental particle formation rates spanning tropospheric sulfuric acid and ammonia abundances, ion production rates, and temperatures |
| Q33463248 | Experimental study of particle formation by ion-ion recombination |
| Q46339955 | Exploring the chemical kinetics of partially oxidized intermediates by combining experiments, theory, and kinetic modeling |
| Q56221437 | Five-S-isotope evidence of two distinct mass-independent sulfur isotope effects and implications for the modern and Archean atmospheres |
| Q58052472 | Forecasting ultrafine particle concentrations from satellite and in situ observations |
| Q89687025 | Formation and growth of sub-3-nm aerosol particles in experimental chambers |
| Q58058926 | Formation and growth of ultrafine particles from secondary sources in Bakersfield, California |
| Q46930710 | Free energy barrier in the growth of sulfuric acid-ammonia and sulfuric acid-dimethylamine clusters |
| Q100415733 | Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
| Q28563967 | Geological support for the Umbrella Effect as a link between geomagnetic field and climate |
| Q58384500 | Global and regional impacts of HONO on the chemical composition of clouds and aerosols |
| Q44866331 | How do organic vapors contribute to new-particle formation? |
| Q56944565 | Hygroscopicity of nanoparticles produced from homogeneous nucleation in the CLOUD experiments |
| Q58070795 | Identification of the biogenic compounds responsible for size-dependent nanoparticle growth |
| Q47157432 | Increased ionization supports growth of aerosols into cloud condensation nuclei. |
| Q56944473 | Influence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleation |
| Q92671736 | Infrared electric field sampled frequency comb spectroscopy |
| Q57885017 | Intercomparison study and optical asphericity measurements of small ice particles in the CERN CLOUD experiment |
| Q38661313 | Introductory lecture: atmospheric chemistry in the Anthropocene |
| Q47809633 | Ion pair particles at the air-water interface |
| Q31101741 | Ion-induced nucleation of pure biogenic particles. |
| Q59326803 | Ion-induced sulfuric acid–ammonia nucleation drives particle formation in coastal Antarctica |
| Q58303374 | Ion–Aerosol Flux Coefficients and the Steady-State Charge Distribution of Aerosols in a Bipolar Ion Environment |
| Q58058794 | Isoprene suppression of new particle formation: Potential mechanisms and implications |
| Q58280649 | Laboratory Characterization of a New Nano-Water-Based CPC 3788 and Performance Comparison to an Ultrafine Butanol-Based CPC 3776 |
| Q91585732 | Long-Term Trend of Gaseous Ammonia Over the United States: Modeling and Comparison With Observations |
| Q57882318 | Long-term analysis of clear-sky new particle formation events and nonevents in Hyytiälä |
| Q46253638 | Mass spectrometry of aerosol particle analogues in molecular beam experiments |
| Q47254146 | Measurement of the nucleation of atmospheric aerosol particles |
| Q28709416 | Midlatitude cooling caused by geomagnetic field minimum during polarity reversal |
| Q36485343 | Mineral dust photochemistry induces nucleation events in the presence of SO2. |
| Q56944572 | Modeling the thermodynamics and kinetics of sulfuric acid-dimethylamine-water nanoparticle growth in the CLOUD chamber |
| Q58707709 | Modulation of Cosmogenic Tritium in Meteoric Precipitation by the 11-year Cycle of Solar Magnetic Field Activity |
| Q37256141 | Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules |
| Q43829556 | Molecular understanding of sulphuric acid-amine particle nucleation in the atmosphere |
| Q37470640 | Molecular-scale evidence of aerosol particle formation via sequential addition of HIO3. |
| Q59750830 | Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors |
| Q39461028 | Multiphase chemistry of atmospheric amines |
| Q34409197 | Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions |
| Q46208083 | New insights into secondary organic aerosol from the ozonolysis of α-pinene from combined infrared spectroscopy and mass spectrometry measurements |
| Q39010725 | New particle formation and growth from methanesulfonic acid, trimethylamine and water. |
| Q58103223 | New particle formation and growth in biomass burning plumes: An important source of cloud condensation nuclei |
| Q58052455 | New particle formation leads to cloud dimming |
| Q59804305 | New perspectives in the study of the Earth's magnetic field and climate connection: The use of transfer entropy |
| Q47556819 | Novel insights on new particle formation derived from a pan-european observing system |
| Q55239993 | Observations of biogenic ion-induced cluster formation in the atmosphere. |
| Q92388818 | On-road emissions of passenger cars beyond the boundary conditions of the real-driving emissions test |
| Q58827945 | Organic molecules on the surface of water droplets – an energetic perspective |
| Q47806290 | Overview: Homogeneous nucleation from the vapor phase-The experimental science |
| Q57882445 | Pan-Arctic aerosol number size distributions: seasonality and transport patterns |
| Q46052466 | Particle formation and growth from oxalic acid, methanesulfonic acid, trimethylamine and water: a combined experimental and theoretical study |
| Q48108623 | Perspective: Aerosol microphysics: From molecules to the chemical physics of aerosols |
| Q52735612 | Photobiological Effects at Earth's Surface Following a 50 pc Supernova. |
| Q58116853 | Precipitation driving of droplet concentration variability in marine low clouds |
| Q63488714 | Processes That Contribute to Decreased Dimethyl Sulfide Production in Response to Ocean Acidification in Subtropical Waters |
| Q44303229 | Quantitative and time-resolved nanoparticle composition measurements during new particle formation |
| Q59144094 | Radiation Transfer Calculations and Assessment of Global Warming by CO2 |
| Q94671784 | Rapid growth of new atmospheric particles by nitric acid and ammonia condensation |
| Q58697490 | Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range |
| Q38925933 | Reaction of SO2 with OH in the atmosphere |
| Q30772027 | Regional and global impacts of Criegee intermediates on atmospheric sulphuric acid concentrations and first steps of aerosol formation |
| Q57689367 | Remarks on Ion Generation for CPC Detection Efficiency Studies in Sub-3-nm Size Range |
| Q44346133 | Resolving the anomalous infrared spectrum of the MeCN-HCl molecular cluster using ab initio molecular dynamics |
| Q58705956 | Robust metric for quantifying the importance of stochastic effects on nanoparticle growth |
| Q57724635 | Role of ammonia in forming secondary aerosols from gasoline vehicle exhaust |
| Q36414716 | Simplified mechanism for new particle formation from methanesulfonic acid, amines, and water via experiments and ab initio calculations |
| Q35774508 | Single-taxon field measurements of bacterial gene regulation controlling DMSP fate. |
| Q29029565 | Solar Influence on Global and Regional Climates |
| Q30938709 | Some characteristics and effects of natural radiation |
| Q38849923 | Spiers Memorial Lecture. Introductory lecture: chemistry in the urban atmosphere |
| Q41827458 | Structural and electrostatic effects at the surfaces of size- and charge-selected aqueous nanodrops. |
| Q58652651 | Sub-3 nm particles observed at the coastal and continental sites in the United States |
| Q58316202 | Sub-micrometer aerosol particles in the upper troposphere/lowermost stratosphere as measured by CARIBIC and modeled using the MIT-CAM3 global climate model |
| Q50502821 | Surface area controlled heterogeneous nucleation. |
| Q57882230 | Technical note: Conversion of isoprene hydroxy hydroperoxides (ISOPOOHs) on metal environmental simulation chamber walls |
| Q56944491 | Temperature uniformity in the CERN CLOUD chamber |
| Q59000831 | The Diurnal Temperature Range for Europe: A Search for Cosmic Ray Forbush Decrease Manifestations and the DTR Periodicities |
| Q59045495 | The Impact of Nonlocal Ammonia on Submicron Particulate Matter and Visibility Degradation in Urban Shanghai |
| Q57689546 | The contribution of organics to atmospheric nanoparticle growth |
| Q36925572 | The effect of acid-base clustering and ions on the growth of atmospheric nano-particles |
| Q42421081 | The effect of carrier gas contaminants on the charging probability of aerosols under bipolar charging conditions |
| Q58241340 | The global extent of the mid stratospheric CN layer: A three-dimensional modeling study |
| Q56002778 | The response of clouds and aerosols to cosmic ray decreases |
| 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. |
| Q58691656 | Theoretical Insights into the Electron Capture Behavior of H₂SO₄···N₂O Complex: A DFT and Molecular Dynamics Study |
| Q59164542 | Variability of aerosol particle number concentrations observed over the western Pacific in the spring of 2009 |
| Q58184916 | Wall effects in smog chamber experiments: A model study |
| Q40152132 | Water droplet excess free energy determined by cluster mitosis using guided molecular dynamics. |
| Q39762789 | Water-soluble ionic species of coarse and fine particulate matter and gas precursor characteristics at urban and rural sites of central Taiwan |
| Q57760528 | What is the solar influence on climate? Overview of activities during CAWSES-II |