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46 results on '"Rörup, Birte"'

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

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

3. Design and performance of the Cluster Ion Counter (CIC).

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

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

6. Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

24. Survival of newly formed particles in haze conditions

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

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

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

28. Role of iodine oxoacids in atmospheric aerosol nucleation

29. Role of iodine oxoacids in atmospheric aerosol nucleation

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

31. Role of iodine oxoacids in atmospheric aerosol nucleation

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

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

34. Molecular understanding of new-particle formation from <i>α</i>-pinene between −50 and +25 °C

35. Enhanced growth rate of atmospheric particles from sulfuric acid

37. Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C

38. Supplementary material to "Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C"

39. Synergistic HNO3–H2SO4–NH3upper tropospheric particle formation

40. Enhanced growth rate of atmospheric particles from sulfuric acid

41. Supplementary material to "Enhanced growth rate of atmospheric particles from sulfuric acid"

42. Molecular understanding of new-particle formation from α-pinene between -50 and +25 ∘C.

43. Molecular understanding of new-particle formation from alpha-pinene between -50 °C and 25 °C.

44. Synergistic particle formation in the upper troposphere by nitric acid, sulfuric acid and ammonia

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

46. Role of iodine oxoacids in atmospheric aerosol nucleation.

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