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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

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

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

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

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

12. Role of sesquiterpenes in biogenic new particle formation

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

14. Global atmospheric particle formation from CERN CLOUD measurements

16. Measurement of the collision rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber

17. Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere

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

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

20. Supplementary material to "Measurement of the rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber"

21. Measurement of the rate coefficients between atmospheric ions and multiply charged aerosol particles in the CERN CLOUD chamber

22. The ion–ion recombination coefficient α: comparison of temperature- and pressure-dependent parameterisations for the troposphere and stratosphere

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

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

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

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

29. Ion-induced nucleation of pure biogenic particles

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

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

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

34. Survival of newly formed particles in haze conditions

35. Chemical composition of nanoparticles from <i>α</i>-pinene nucleation and the influence of isoprene and relative humidity at low temperature

37. The driving factors of new particle formation and growth in the polluted boundary layer

38. New particle formation from sulfuric acid and ammonia: nucleation and growth model based on thermodynamics derived from CLOUD measurements for a wide range of conditions

39. Molecular understanding of sulphuric acid–amine particle nucleation in the atmosphere

40. Supplementary material to "Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature"

41. Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature

42. Role of iodine oxoacids in atmospheric aerosol nucleation

43. Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature

45. Molecular understanding of new-particle formation from α-pinene between −50 and +25 °C

47. Supplementary material to "The driving factors of new particle formation and growth in the polluted boundary layer"

48. Molecular characterization of ultrafine particles using extractive electrospray time-of-flight mass spectrometry

49. Role of sulphuric acid, ammonia and galactic cosmic rays in atmospheric aerosol nucleation

50. Determination of the collision rate coefficient between charged iodic acid clusters and iodic acid using the appearance time method

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