ACPD Atmospheric Chemistry and Physics Discussions ACPD 1680-7375 Copernicus GmbH Göttingen, Germany 10.5194/acpd-10-17609-2010 Variability of aerosol vertical distribution in the Sahel Cavalieri O. 1 Cairo F. 1 Fierli F. 1 Di Donfrancesco G. 2 Snels M. 1 Viterbini M. 1 Cardillo F. 1 Chatenet B. 3 Formenti P. 3 Marticorena B. 3 Rajot J. L. 4 Consiglio Nazionale delle Ricerche-Istituto di Scienze dell'Atmosfera e del Clima, Rome, Italy Ente per le Nuove Tecnologie Energia e Ambiente, Frascati, Italy LISA, Universités Paris Est-Paris Diderot-Paris 7, CNRS, Créteil, France IRD-UMR 211 Bioemco, Niamey, Niger 21 07 2010 10 7 17609 17655 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys-discuss.net/10/17609/2010/acpd-10-17609-2010.html The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/17609/2010/acpd-10-17609-2010.pdf

We present and discuss ground-based and satellite observations of aerosol optical properties over Sahelian Africa for the years 2006, 2007 and 2008. <br><br> This study combines data acquired by three ground-based micro lidar systems located in Banizoumbou (Niger), Cinzana (Mali) and M'Bour (Senegal) in the framework of the African Monsoon Multidisciplinary Analysis (AMMA), by the AEROsol RObotic NETwork (AERONET) sun-photometers and by the space-based Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) onboard Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO). <br><br> The 2006 seasonal pattern of the aerosols vertical distribution is presented. It shows the presence of aerosol mainly confined in the lower levels of the atmosphere during the dry season, with the aerosol layer increasing in vertical extension and absolute values in spring, reaching the largest values in summer in correspondence with a progressive clearing up of the atmosphere at the lowermost levels. <br><br> Aerosol produced by biomass burning are observed mainly during the dry season, when north-easterly air masses pass over large biomass burning areas before recirculating over the measurement sites. This kind of aerosol is present mainly in layers between 2 and 6 km of altitude, although episodically it may show also below 2 km, as observed in Banizoumbou (Niger) in 2006. Biomass burning aerosol is also observed during spring when air masses originating from North and East Africa pass over sparse biomass burning sources, and during summer when biomass burning aerosol is transported from the southern part of the continent by the monsoon flow. <br><br> The summer season on the whole is characterized by a large presence of desert dust along the entire Sahelian region, widespread in altitude with Aerosol Optical Depths above 0.2. <br><br> The interannual variability in the three year monitoring period is not very significant. An analysis of the aerosol transport pathways, aiming at detecting the main source regions, revealed that air originated from the Saharan desert is present all year long and it is observed in the lower levels of the atmosphere at the beginning and at the end of the year. In the central part of the year it extends upward and the lower levels are less affected by air masses from Saharan desert when the monsoon flow carries inland air from the Guinea Gulf and Southern Hemisphere. Biomass burning is mainly confined in the higher layers and observable in winter and in autumn.

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