Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Joseph L. Woo"'
Publikováno v:
Atmosphere, Vol 11, Iss 4, p 358 (2020)
The proper characterization of aqueous brown carbon (BrC) species, their formation, and their light absorbance properties is critical to understanding the aggregate effect that they have on overall atmospheric aerosol climate forcing. The contributio
Externí odkaz:
https://doaj.org/article/07263fda730841c1b2c6787a33cc7da2
Publikováno v:
Atmosphere, Vol 10, Iss 11, p 666 (2019)
Chemical processing of organic material in aqueous atmospheric aerosols and cloudwater is known to form secondary organic aerosols (SOA), although the extent to which each of these processes contributes to total aerosol mass is unclear. In this study
Externí odkaz:
https://doaj.org/article/6fa722ed5ea14766b60713c07e1fb11c
Publikováno v:
ACS Earth and Space Chemistry. 5:1902-1915
Autor:
Joseph L. Woo, Heidi P. Hendrickson, Daisy N. Grace, Emily N. Lugos, Daniel R. Griffith, Melissa M. Galloway, Shiqing Ma
Publikováno v:
ACS Earth and Space Chemistry. 4:1104-1113
The contribution of organic aerosol from biomass burning is poorly constrained, and the lack of consensus regarding its overall contribution to global radiative forcing leads to significant uncerta...
Publikováno v:
ACS Earth and Space Chemistry. 3:1208-1215
Dark-chemistry products of ammonium sulfate (AS) and methylglyoxal (MG) have been observed to be surface-active, resulting in changes to solution surface tension with relatively small amounts of or...
Publikováno v:
Atmosphere
Volume 11
Issue 4
Atmosphere, Vol 11, Iss 358, p 358 (2020)
Volume 11
Issue 4
Atmosphere, Vol 11, Iss 358, p 358 (2020)
The proper characterization of aqueous brown carbon (BrC) species, their formation, and their light absorbance properties is critical to understanding the aggregate effect that they have on overall atmospheric aerosol climate forcing. The contributio
Publikováno v:
Atmosphere, Vol 10, Iss 11, p 666 (2019)
Atmosphere
Volume 10
Issue 11
Atmosphere
Volume 10
Issue 11
Chemical processing of organic material in aqueous atmospheric aerosols and cloudwater is known to form secondary organic aerosols (SOA), although the extent to which each of these processes contributes to total aerosol mass is unclear. In this study
Publikováno v:
Atmospheric Measurement Techniques, Vol 12, Pp 3395-3402 (2019)
We present a concept for enhancing the concentration of charged submicron aerosol particles in a continuous flow stream using in situ electrostatic focusing. It is proposed that electrostatic focusing can enable the continuous, isothermal concentrati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ff0d38e79ee5ada6b44217358478b3b6
https://www.atmos-meas-tech.net/12/3395/2019/
https://www.atmos-meas-tech.net/12/3395/2019/
Autor:
Joseph L. Woo, V. F. McNeill
Publikováno v:
Geoscientific Model Development, Vol 8, Iss 6, Pp 1821-1829 (2015)
There is increasing evidence that the uptake and aqueous processing of water-soluble volatile organic compounds (VOCs) by wet aerosols or cloud droplets is an important source of secondary organic aerosol (SOA). We recently developed GAMMA (Gas–Aer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b402ce7e934e3c3722f0adbc22e84fd
https://www.geosci-model-dev.net/8/1821/2015/
https://www.geosci-model-dev.net/8/1821/2015/