Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Kerrigan P. Cain"'
Publikováno v:
Aerosol Science and Technology. 54:941-957
Volatility is one of the most important physical properties of organic aerosol (OA), as it determines the partitioning of its components between the vapor and particulate phases. Despite their atmo...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02c48a9d74bf0c27832ab82bb71fb3b3
https://doi.org/10.1080/02786826.2020.1748172
https://doi.org/10.1080/02786826.2020.1748172
Autor:
Thomas Brubaker, Ryan C. Sullivan, Bailey B. Bowers, Leif G. Jahn, Kerrigan P. Cain, Lydia G. Jahl, Michael Polen, William D. Fahy, Sara Graves
Publikováno v:
Science Advances
Ability of biomass-burning smoke particles to glaciate clouds increases as the plume undergoes atmospheric dilution and aging.
Ice-nucleating particles (INPs) in biomass-burning aerosol (BBA) that affect cloud glaciation, microphysics, precipita
Ice-nucleating particles (INPs) in biomass-burning aerosol (BBA) that affect cloud glaciation, microphysics, precipita
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::005e89190ae4904c622a520cd18237a7
https://doi.org/10.1126/sciadv.abd3440
https://doi.org/10.1126/sciadv.abd3440
Autor:
Spyros N. Pandis, Yanwei Li, Antonios Tasoglou, Evangelia Kostenidou, Peishi Gu, Kerrigan P. Cain, Aikaterini Liangou, Leif G. Jahn
Publikováno v:
Atmospheric Environment. 176:103-109
Cooking organic aerosol (COA) is potentially a significant fraction of organic particulate matter in urban areas. COA chemical aging experiments, using aerosol produced by grilling hamburgers, took place in a smog chamber in the presence of UV light
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d907dc8f08ca81ab5f0e1f820c6dc973
https://doi.org/10.1016/j.atmosenv.2017.11.035
https://doi.org/10.1016/j.atmosenv.2017.11.035
Publikováno v:
Aerosol and Air Quality Research. 21:200511
The hygroscopicity and oxidation level of secondary organic aerosol (SOA) produced in an atmospheric simulation chamber were measured as a function of volatility. The experimental setup combines thermodenuding, isothermal dilution, aerosol mass spect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf6019899fd497e2ce0971b5b4523ab5
https://doi.org/10.4209/aaqr.2020.08.0511
https://doi.org/10.4209/aaqr.2020.08.0511
