A study on the direct effect of anthropogenic aerosols on near surface air temperature over Southeastern Europe during summer 2000 based on regional climate modeling

Therefore it is useful to utilize the available archive of ship-based AOD measurements over the oceans ac- quired within the framework of Maritime Aerosol Network (Smirnov et

The model has been used to study the impact of aerosol direct radiative e ff ect on East Asian climate (Zhang et al., 2012a), direct radiative forcing of anthropogenic aerosols (Bond

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

The Antarctic near-coastal sub-micrometre aerosol particle features in summer were characterised based on measured data on aerosol hygroscopicity, size distributions, volatility

For the US summer mean, the simulated ammonia surface concentrations increase by 8.8 % from 2008 to 2012 due to the anthropogenic emissions changes, compared to the 29 % decrease

Measurements of aerosol chemical composition and aerosol optical depth in the Nepal Himalaya have clearly shown the build up of aerosols in the pre-monsoon season during the winter

(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

Because of the increas- ing the speed of the decomposition of the anhydrite, together with the growth of the temperature of casting the bronze to the plaster mould, the gases