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Source apportionment for African dust outbreaks over the Western Mediterranean using the HYSPLIT model
Authors:M Escudero  AF Stein  RR Draxler  X Querol  A Alastuey  S Castillo  A Avila
Institution:1. Department of Applied Physics, Politechnical School of Huesca, University of Saragossa, Carretera de Cuarte, s/n, 22071, Huesca, Spain;2. Institute of Environmental Assessment and Water Research, IDAEA-CSIC, C/Jorge Girona Salgado, 18-26, 08034, Barcelona, Spain;3. Earth Resources & Technology, on assignment to National Oceanic and Atmospheric Administration, Air Resources Laboratory, 1315 East West Highway, Silver Spring, MD, 20910, USA;4. National Oceanic and Atmospheric Administration, Air Resources Laboratory, 1315 East West Highway, Silver Spring, MD, 20910, USA;5. Centre for Ecological Research and Forestry Applications (CREAF), Building C, Autonomous University of Barcelona, 08193, Bellaterra (Barcelona), Spain
Abstract:A source apportionment technique has been applied to determine the geographical distribution of emissions in Northern Africa contributing to dust outbreaks that yield high PM10 levels at Spanish regional background stations. Seven dust episodes have been analyzed in this study. Total suspended particles have been sampled and chemically analyzed for these events at La Castanya background station (Montseny, NE Spain) and differences in the composition of airborne dust have been studied. The dominant role of northern and western source areas (Tunisia, Algeria, Mauritania and the Western Sahara) contrasted with the negligible contribution of major emission source areas such as the Bodelé depression, Libya, Niger, and Sudan. During the simulated events using the dust module of the HYSPLIT model, material from the latter regions is persistently transported across the Atlantic but not towards Western Europe. As a consequence, the composition of the dust turned out to be quite homogeneous since the mixing of dust occurs from various source areas with similar chemical composition. However, differences in Ca/Al ratios have been found in a number of samples that are mainly explained by vertical transport segregation of clay minerals (relatively richer in Al) from coarser dust particles (Ca-carbonate).
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