International audienceIn this study, we characterize the CCN activity of the water-soluble organics in biomass burning aerosol. The aerosol after collection upon filters is dissolved in water using sonication. Hydrophobic and hydrophilic components are fractionated from a portion of the original sample using solid phase extraction, and subsequently desalted. The surface tension and CCN activity of these different samples are measured with a KSV CAM 200 goniometer and a DMT Streamwise Thermal Gradient CCN Counter, respectively. The measurements show that the strongest surfactants are isolated in the hydrophobic fraction, while the hydrophilics exhibit negligible surface tension depression. The presence of salts (primarily (NH4)2SO4) in the h...
Organic material, about half of which is water soluble, constitutes nearly 80% of the wet-season aer...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
The composition of aerosol from cloud droplets differs from that below cloud. Its implications for t...
International audienceIn this study, we characterize the CCN activity of the water-soluble organics ...
International audienceThis study presents a new method, Köhler Theory Analysis (KTA), to infer the m...
International audienceThe CCN properties, surfactant characteristics, and droplet growth kinetics of...
International audienceThe aerosol in the Amazon basin is dominated throughout the year by organic ma...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
This paper describes the effect of the presence of water-soluble organic compounds (WSOC) in aerosol...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
Aerosols have significant impacts on earth's climate and hydrological cycle. They can directly refl...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
An existing method for the measurement of atmospheric gaseous species was modified to collect data o...
Organic material, about half of which is water soluble, constitutes nearly 80% of the wet-season aer...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
The composition of aerosol from cloud droplets differs from that below cloud. Its implications for t...
International audienceIn this study, we characterize the CCN activity of the water-soluble organics ...
International audienceThis study presents a new method, Köhler Theory Analysis (KTA), to infer the m...
International audienceThe CCN properties, surfactant characteristics, and droplet growth kinetics of...
International audienceThe aerosol in the Amazon basin is dominated throughout the year by organic ma...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
This paper describes the effect of the presence of water-soluble organic compounds (WSOC) in aerosol...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
Aerosols have significant impacts on earth's climate and hydrological cycle. They can directly refl...
We investigate the CCN activity of freshly emitted biomass burning particles and their hygroscopic g...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
An existing method for the measurement of atmospheric gaseous species was modified to collect data o...
Organic material, about half of which is water soluble, constitutes nearly 80% of the wet-season aer...
Cloud formation characteristics of the water-soluble organic fraction (WSOC) of secondary organic ae...
The composition of aerosol from cloud droplets differs from that below cloud. Its implications for t...