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pro vyhledávání: '"Anthoula D. Drosatou"'
Secondary organic aerosol (SOA) constitutes a major fraction of the total organic aerosol (OA) in the atmosphere. SOA is formed by the partitioning onto pre-existent particles of low vapor pressure products of the oxidation of volatile, intermediate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bf2c061fc782e904bae93c32fb06f3c
https://doi.org/10.5194/egusphere-egu21-10088
https://doi.org/10.5194/egusphere-egu21-10088
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 973-986 (2019)
Factor analysis of aerosol mass spectrometer measurements (organic aerosol mass spectra) is often used to determine the sources of organic aerosol (OA). In this study we aim to gain insights regarding the ability of positive matrix factorization (PMF
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b6a3f9fcb5309eab5c2a6d79d7b3c426
https://www.atmos-chem-phys.net/19/973/2019/
https://www.atmos-chem-phys.net/19/973/2019/