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1. Oxidized organic molecules in the tropical free troposphere over Amazonia

2. Atmospheric new particle formation from the CERN CLOUD experiment

3. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

4. Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation

5. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range

6. Constraining nucleation, condensation, and chemistry in oxidation flow reactors using size-distribution measurements and aerosol microphysical modeling

7. Nitrate Radicals Suppress Biogenic New Particle Formation from Monoterpene Oxidation

8. Neutral molecular cluster formation of sulfuric acid dimethylamine observed in real time under atmospheric conditions

9. The role of low-volatility organic compounds in initial particle growth in the atmosphere

10. The effect of acid-base clustering and ions on the growth of atmospheric nano-particles.

11. Opinion: The strength of long-term comprehensive observations to meet multiple grand challenges in different environments and in the atmosphere

12. Rapid growth of new atmospheric particles by nitric acid and ammonia condensation

13. Role of sesquiterpenes in biogenic new particle formation

14. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules

15. Supplementary material to "Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules"

16. Observations of Diurnal to Weekly Variations of Monoterpene-Dominated Fluxes of Volatile Organic Compounds from Mediterranean Forests: Implications for Regional Modeling

18. Organosulfates as Tracers for Secondary Organic Aerosol (SOA) Formation from 2‑Methyl-3-Buten-2-ol (MBO) in the Atmosphere

20. Analysis of formaldehyde fluxes above a Ponderosa Pine forest measured via eddy-covariance

24. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

25. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere

26. Oxidized organic molecules in the tropical free troposphere over Amazonia

27. Opinion: The strength of long-term comprehensive observations to meet multiple grand challenges at different environments and in the atmosphere

28. Nitrate radicals suppress biogenic new particle formation from monoterpene oxidation

29. Global atmospheric particle formation from CERN CLOUD measurements

30. Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation

31. Temperature, humidity, and ionisation effect of iodine oxoacid nucleation

33. NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere

34. Global budget of methanol: Constraints from atmospheric observations

35. Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity

36. Measurement report: Long-range transport and the fate of dimethyl sulfide oxidation products in the free troposphere derived from observations at the high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes

38. Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules.

39. Supplementary material to "Measurement report: Molecular-level investigation of atmospheric cluster ions at the tropical high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes"

40. Measurement report: Molecular-level investigation of atmospheric cluster ions at the tropical high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes

41. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

43. Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions

44. Measurement Report: Long-range transport and fate of DMS-oxidation products in the free troposphere derived from observations at the high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes

45. High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures

46. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

47. Supplementary material to "An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles"

49. Oxidation Products of Biogenic Emissions Contribute to Nucleation of Atmospheric Particles

50. Molecular understanding of atmospheric particle formation from sulfuric acid and large oxidized organic molecules

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