Du Preez, David JeanBencherif, HassanBègue, NelsonClarisse, LievenHoffman, Rebecca FWright, Caradee Yael2020-10-152020-10-152020-10-15Du Preez, D.J., Bencherif, H., Begue, N. et al. 2020, 'Investigating the large-scale transport of a volcanic plume and the impact on a secondary site', Atmosphere, vol. 11, no. 5, art. 548, pp. 1-11.2073-4433 (online)10.3390/atmos11050548http://hdl.handle.net/2263/76481Volcanic plumes can be transported across vast distances and can have an impact on solar ultraviolet radiation (UVR) reaching the surface due to the scattering and absorption caused by aerosols. The dispersion of the volcanic plume from the Puyehue-Cordón Caulle volcanic complex (PCCVC) eruption was investigated to determine the effect on aerosol loading at Cape Point, South Africa. The eruption occurred on 4 June 2011 and resulted in a plume reaching a height of between 9 and 12 km and was dispersed across the Southern Hemisphere. Satellite sulphur dioxide (SO2) observations and a dispersion model showed low concentrations of SO2 at the secondary site. However, satellite observations of volcanic ash and ground-based aerosol measurements did show increases between 10 and 20 June 2011 at the secondary site. Furthermore, there was good agreement with the dispersion model results and observations from satellites with most of the plume located between latitudes 40◦–60◦ South.en© 2020 by the authors. Licensee: MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.AerosolsSulphur dioxideFLEXPARTPlume transportVolcanic eruptionUltraviolet radiation (UVR)Volcanic plumePuyehue-Cordón Caulle volcanic complex (PCCVC)Article