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36. Unraveling the sources of atmospheric organic aerosols over the Arabian Sea: Insights from the stable carbon and nitrogen isotopic composition P. Bikkina et al. https://doi.org/10.1016/j.scitotenv.2022.154260
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48. Volatility of Secondary Organic Aerosol from β-Caryophyllene Ozonolysis over a Wide Tropospheric Temperature Range L. Gao et al. https://doi.org/10.1021/acs.est.3c01151
49. Physical state of 2-methylbutane-1,2,3,4-tetraol in pure and internally mixed aerosols J. Lessmeier et al. https://doi.org/10.5194/acp-18-15841-2018
50. Molecular composition and gas-particle partitioning of indoor cooking aerosol: Insights from a FIGAERO-CIMS and kinetic aerosol modeling C. Masoud et al. https://doi.org/10.1080/02786826.2022.2133593
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52. Highly time-resolved chemical speciation and source apportionment of organic aerosol components in Delhi, India, using extractive electrospray ionization mass spectrometry V. Kumar et al. https://doi.org/10.5194/acp-22-7739-2022
53. Impact of organic molecular structure on the estimation of atmospherically relevant physicochemical parameters G. Isaacman-VanWertz & B. Aumont https://doi.org/10.5194/acp-21-6541-2021
54. Modeling Volatility-Based Aerosol Phase State Predictions in the Amazon Rainforest Q. Rasool et al. https://doi.org/10.1021/acsearthspacechem.1c00255
55. The complex composition of organic aerosols emitted during burning varies between Arctic and boreal peat E. Schneider et al. https://doi.org/10.1038/s43247-024-01304-y
56. Particulate matter (PM) episodes at a suburban site in Hong Kong: evolution of PM characteristics and role of photochemistry in secondary aerosol formation Y. Qin et al. https://doi.org/10.5194/acp-16-14131-2016
57. Secondary organic aerosols from oxidation of 1-methylnaphthalene: Yield, composition, and volatility W. Xiang et al. https://doi.org/10.1016/j.scitotenv.2024.170379
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67. Relative humidity effect on the formation of highly oxidized molecules and new particles during monoterpene oxidation X. Li et al. https://doi.org/10.5194/acp-19-1555-2019
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