Aerosol size distribution and radiative forcing response to anthropogenically driven historical changes in biogenic secondary organic aerosol formation

We find that the variability in the CCN concentrations in the central Amazon is mostly driven by aerosol particle number concentration and size distribution, while variations in

Here we simulate the air quality and radiative forcing (RF) impacts of changes in ozone, methane, and sulfate from halving anthropogenic NMVOC emissions globally and from.. 10

updraft velocity for the Koelher-Aero-Acc simulations using medium and high aerosol concentrations but after this time period the e ffi cient depletion of accumulation mode

Predicted seasonal average SOA concentrations due to contributions from different precursors in (a) spring (March, April and May), (b) summer (June, July and August), (c)

fire aerosol radiative effect (RE) at TOA, radiative effects due to aerosol–radiation interactions (REari), due to aerosol–cloud interactions (REaci), surface-albedo changes (REsac)

In this study, we analyzed number concentration and size distribution of aerosol particles, together with the mass concentration and chemical composition of UFPs and PM 1

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..

(a) MODIS mean aerosol optical depth at 550 nm over Amazonia during the dry season (b) and mean direct aerosol radiative forcing of aerosols (DARF24h) during the peak of the