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7. Formation and temperature dependence of highly oxygenated organic molecules (HOMs) from Δ3-carene ozonolysis.

9. Recent advances in understanding secondary organic aerosol formation from ozonolysis of Δ3-carene and other monoterpenes

11. Natural Marine Precursors Boost Continental New Particle Formation and Production of Cloud Condensation Nuclei

14. Gas-to-Particle Partitioning of Products from Ozonolysis of Δ3-Carene and the Effect of Temperature and Relative Humidity

16. Formation and temperature dependence of Highly Oxygenated Organic Molecules (HOM) from Δ³-carene ozonolysis.

19. Supplementary material to "Towards a mechanistic description of autoxidation chemistry: from precursors to atmospheric implications"

20. Towards a mechanistic description of autoxidation chemistry: from precursors to atmospheric implications

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

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

23. The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system

25. Measurement report: Black carbon properties and concentrations in southern Sweden urban and rural air – the importance of long-range transport

29. The effect of temperature and relative humidity on secondary organic aerosol formation from ozonolysis of Δ3-careneElectronic supplementary information (ESI) available: Placement and sampling cycles of instruments, wall-loss correction, experimental details, background concentration of sulfuric acid, evolution in moderately oxygenated species, details of the offline analysis, time-evolution plots of ozonolysis products (PDF). See DOI: https://doi.org/10.1039/d3ea00128h

30. Towards automated inclusion of autoxidation chemistry in models: from precursors to atmospheric implicationsElectronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ea00054d

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

33. Secondary aerosol formation in marine Arctic environments: a model measurement comparison at Ny-Ålesund

34. Towards a mechanistic description of autoxidation chemistry: from precursors to atmospheric implications.

35. Supplementary material to "Measurement Report: Small effect of regional sources on black carbon properties and concentrations in Southern Sweden background air"

36. Measurement Report: Small effect of regional sources on black carbon properties and concentrations in Southern Sweden background air

37. Secondary aerosol formation in marine Arctic environments : a model measurement comparison at Ny-Ålesund

39. De unga gör helt rätt när de stämmer staten

40. Supplementary material to "Secondary aerosol formation in marine Arctic environments: A model measurement comparison at Ny-Ålesund"

41. Secondary aerosol formation from dimethyl sulfide-improved mechanistic understanding based on smog chamber experiments and modelling

42. The Aerosol Chase:A continental lagrangian experiment

44. New Particle Formation and Growth from Dimethyl Sulfide Oxidation by Hydroxyl Radicals

46. Measurement Report: Small effect of regional sources on black carbon properties and concentrations in Southern Sweden background air.

47. A modelling study of OH, NO3 and H2SO4 in 2007–2018 at SMEAR II, Finland: analysis of long-term trends

49. Sensitivity of spatial aerosol particle distributions to the boundary conditions in the PALM model system 6.0

50. Supplementary material to "Sensitivity of spatial aerosol particle distributions to the boundary conditions in the PALM model system 6.0"

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