CCN activation and cloud processing in sectional aerosol models with low size resolution

P ¨oschl, U.: Aerosol- and updraft-limited regimes of cloud droplet formation: influence of par- ticle number, size and hygroscopicity on the activation of cloud condensation

1 World Economic Outlook (WEO), abril de 2011. 2 Polity IV é um índice calculado e divulgado para uma série de países, que pode ser encontrado neste endereço

When droplets condensed on CCN grow large enough to be distinguished from non- activated nuclei, the cloud droplets’ size distribution calculated by the parcel model is assigned to

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,

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..

Overall size statistics of the background aerosol particles (left), cloud ice residues (middle) and cloud droplet residues (right) detected with the SPLAT instrument (upper row) and

The structure of the remelting zone of the steel C90 steel be- fore conventional tempering consitute cells, dendritic cells, sur- rounded with the cementite, inside of

In the current study, the intracellular PC-to-PE ratio was also associated with the size of the lipid droplets secreted into the medium: the size of droplets secreted from