Carbonaceous particles and their organic component are one of the major combustion by-products and they are recognized to play a relevant role in radiative transfer, air quality, and human health, due to their fine-submicrometric nature. These effects are magnified by transboundary air masses transport of natural fires plumes or anthropogenic emissions from domestic heating and industrial activities, affecting not only the source areas. In fact, analysis on snow samples from different arctic sites revealed the presence of carbonaceous particulate matter, with biomass burning identified as responsible for more than 90% of these particles. As a consequence of this deposition, snow albedo variations are added to the other factors influencing Earth's radiative budget. For these reasons, there is a growing interest toward the above-mentioned arguments, but there is also a need to assess the role of carbonaceous particles [1] and to review the different measurements techniques, highlighting their limitations and uncertainties [2]. The papers included in this special issue improve the comprehension of processes involving carbonaceous particles considering them under different points of view because both experimental and modeling approaches are examined. S. Byčenkien˙ e et al., starting from one-year continuous aethalometer measurements of black carbon (BC) content at a background site in Lithuania, were able to study the transport of different air masses. In particular, air masses from Ukraine and the volcanic plume from the Grimsvotn eruption were characterized by estimating the alpha absorp-tion parameter at shorter and longer wavelengths. In this way, they demonstrate that grass burning was the major source of carbonaceous particles in the atmosphere. Moreover, new secondary particle formation from volcanic gas emissions, occurred within the lower troposphere, was detected even at a large distance from the eruption site. Y. Aboel Fetouh et al. use long-term series of parameters from the Tropospheric Emission Spectrometer (TES) on board the Aura satellite to assess the dominant component below the inversion layer. Time series analysis, autocorrela-tions, and cross correlations were useful to understand the connections between those parameters and their local effect. In particular, they were able to identify different pollution episodes known as Black Clouds over Cairo city and their climatic origin, confirming biomass burning to be a serious problem affecting air quality in that area. J. L. Hand et al. aggregated OC and EC data from 2007 to 2010 at over 300 sites from the rural/remote IMPROVE (interagency monitoring of protected visual environments) network and the Environmental Protection Agency's urban chemical speciation network to characterize the spatial and seasonal patterns in rural and urban carbonaceous aerosols. From the interpolation of these data, they found large spatial patterns from which local and regional impacts of carbonaceous aerosols across the United States were inferred.