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Introduction

The aerosol climatology was derived from the CAMS interim Reanalysis and its control run (Flemming et al. 2017) as described in Bozzo et al. (2019). The data set is based on the modelled aerosol mixing ratios of the control run, which were scaled to match the Aerosol Optical Depth (AOD) analyses of the CAMS interim Reanalysis (Data assimilation of MODIS AOD). It contains monthly mean 3D mass mixing ratios of desert dust (3 size bins), seas salt (3 size bins), organic matter, black carbon and sulphate as represented by the IFS-AER aerosol scheme (Remy et al. 2019) .

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Rémy, S., Kipling, Z., Flemming, J., Boucher, O., Nabat, P., Michou, M., Bozzo, A., Ades, M., Huijnen, V., Benedetti, A., Engelen, R., Peuch, V.-H., and Morcrette, J.-J.: Description and evaluation of the tropospheric aerosol scheme in the European Centre for Medium-Range Weather Forecasts (ECMWF) Integrated Forecasting System (IFS-AER, cycle 45R1), Geosci. Model Dev., 12, 4627–4659, https://doi.org/10.5194/gmd-12-4627-2019, 2019.

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This document has been produced in the context of theCopernicus Atmosphere Monitoring Service (CAMS).

The activities leading to these results have been contracted by the European Centre for Medium-Range Weather Forecasts, operator of CAMS on behalf of the European Union (Delegation Agreement signed on 11/11/2014 and Contribution Agreement signed on 22/07/2021). All information in this document is provided "as is" and no guarantee or warranty is given that the information is fit for any particular purpose.

The users thereof use the information at their sole risk and liability. For the avoidance of all doubt , the European Commission and the European Centre for Medium - Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view.

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