Observations of high droplet number concentrations in Southern Ocean boundary layer clouds

In that paper, several cloud fields with the same stochastic properties as real clouds are generated assuming variable cloud tops, vertical profile of water droplet, mixed phase,

We use a global aerosol microphysics model to estimate the effect of particle formation through activation nucleation in the boundary layer (BL) on cloud droplet num- ber

The number of aerosols that eventually activate into cloud droplets depends on the aerosol concentration, size distribution and chemical properties and on the updraft ve- locity,

Weekly cycles have been analysed in surface observations of sulfur dioxide and sul- fate concentrations, satellite observations of aerosol optical depth, cloud properties (cloud

The second nucleation mechanism, organic nucleation rate, is presented in sense of kinetic nucleation with the assumption that new particles are formed through colli- sions

aerosol optical depth (AOD) of the atmosphere, acoustic sounding of the boundary layer, laser sensing of the aerosol content in the troposphere and stratosphere, mea- surement of

Average tropospheric OH concentration, estimated methane lifetime, global mean cloud droplet number concentration (CDNC), changes in the global-mean total and cloud cover and

In simulation SCAV- w the scavenging processes within the orographic cloud im- pact the aerosol size distribution by reducing the number and mass of unactivated aerosol particles..