The rate at which freshly formed secondary aerosol particles grow is an important factor in determining their climate impacts. The growth rate of atmospheric nanoparticles may be affected by particle-phase oligomerization and decomposition of condensing organic molecules. We used the Model for Oligomerization and Decomposition in Nanoparticle Growth (MODNAG) to investigate the potential atmospheric significance of these effects. This was done by conducting multiple simulations with varying reaction-related parameters (volatilities of the involved compounds and reaction rates) using both artificial and ambient measured gas-phase concentrations of organic vapors to define the condensing vapors. While our study does not aim at providing inform...
Atmospheric new particle formation (NPF) is a key source of ambient ultrafine particles that may con...
The oxidation of biogenic volatile organic compounds (BVOCs) gives a range of products, from semi-vo...
The probability that freshly nucleated nanoparticles can survive to become cloud condensation nuclei...
The rate at which freshly formed secondary aerosol particles grow is an important factor in determin...
Climatic effects of newly-formed atmospheric secondary aerosol particles are to a large extent deter...
Particles formed in the atmosphere via nucleation provide about half the number of atmospheric cloud...
Particles formed in the atmosphere via nucleation provide about half the number of atmospheric cloud...
Johnston, Murray V., IIIAtmospheric nanoparticles are suspended particulate matter with diameters of...
Atmospheric new particle formation occurs frequently in the global atmosphere and may play a crucial...
International audienceA modelling study investigating the formation of organic particles from inorga...
A new aerosol dynamics model (DMANx) has been developed that simulates aerosol size/composition dist...
We used the Aerosol Dynamics gas- and particle-phase chemistry model for laboratory CHAMber studies ...
We used the Aerosol Dynamics gas- and particle-phase chemistry model for laboratory CHAMber studies ...
Atmospheric new particle formation (NPF) is a key source of ambient ultrafine particles that may con...
New particle formation (NPF) represents the first step in the complex processes leading to formation...
Atmospheric new particle formation (NPF) is a key source of ambient ultrafine particles that may con...
The oxidation of biogenic volatile organic compounds (BVOCs) gives a range of products, from semi-vo...
The probability that freshly nucleated nanoparticles can survive to become cloud condensation nuclei...
The rate at which freshly formed secondary aerosol particles grow is an important factor in determin...
Climatic effects of newly-formed atmospheric secondary aerosol particles are to a large extent deter...
Particles formed in the atmosphere via nucleation provide about half the number of atmospheric cloud...
Particles formed in the atmosphere via nucleation provide about half the number of atmospheric cloud...
Johnston, Murray V., IIIAtmospheric nanoparticles are suspended particulate matter with diameters of...
Atmospheric new particle formation occurs frequently in the global atmosphere and may play a crucial...
International audienceA modelling study investigating the formation of organic particles from inorga...
A new aerosol dynamics model (DMANx) has been developed that simulates aerosol size/composition dist...
We used the Aerosol Dynamics gas- and particle-phase chemistry model for laboratory CHAMber studies ...
We used the Aerosol Dynamics gas- and particle-phase chemistry model for laboratory CHAMber studies ...
Atmospheric new particle formation (NPF) is a key source of ambient ultrafine particles that may con...
New particle formation (NPF) represents the first step in the complex processes leading to formation...
Atmospheric new particle formation (NPF) is a key source of ambient ultrafine particles that may con...
The oxidation of biogenic volatile organic compounds (BVOCs) gives a range of products, from semi-vo...
The probability that freshly nucleated nanoparticles can survive to become cloud condensation nuclei...