Status: this preprint was under review for the journal ACP but the revision was not accepted.
Analysis of the atmospheric composition during the summer 2013 over the Mediterranean area using the CHARMEX measurements and the CHIMERE model
L. Menut,S. Mailler,G. Siour,B. Bessagnet,S. Turquety,G. Rea,R. Briant,M. Mallet,J. Sciare,and P. Formenti
Abstract. The ADRIMED campaign provides measurements of all key parameters regarding atmospheric composition in the Mediterranean area during the summer 2013. This is an opportunity to quantify the ability of current models to adequately represent the atmospheric composition in this complex region, which is influenced by anthropogenic emissions from Europe, Africa, the Middle-East and from shipping activities as well as mineral dust emissions mostly from the arid areas in Africa, sea-salt emissions, biomass burning emissions and biogenic emissions from the vegetation. The CHIMERE model in its present version is a chemistry-transport model which takes into account all these processes. We show here by simulating the period from 5 June to 15 July 2013 with the CHIMERE model and comparing the results to both routine and specific ADRIMED measurements that this model allows an adequate representation the atmospheric composition over the western Mediterranean, in terms of ozone concentration, particulate matter (PM) and aerosol optical depth (AOD). It is also shown that the concentrations of PM on all the considered area is dominated by mineral dust, even though local dust emissions in Europe are certainly overestimated by the model. A comparison with sulphate concentrations at Cape Corsica exhibits some discrepancies related to the regridding of shipping emissions.
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LMD, Laboratoire de Météorologie Dynamique, UMR CNRS 8539, Ecole Polytechnique, Ecole Normale Supérieure, Université P. M. Curie, Ecole Nationale des Ponts et Chaussées, Palaiseau, France
LMD, Laboratoire de Météorologie Dynamique, UMR CNRS 8539, Ecole Polytechnique, Ecole Normale Supérieure, Université P. M. Curie, Ecole Nationale des Ponts et Chaussées, Palaiseau, France
G. Siour
LISA, Laboratoire Inter-Universitaire des Systèmes Atmosphériques, UMR CNRS 7583, Université Paris Est Créteil et Université Paris Diderot, Institut Pierre Simon Laplace, Créteil, France
B. Bessagnet
INERIS, Institut National de l'Environnement Industriel et des Risques, Verneuil en Halatte, 60550, Parc Technologique ALATA, France
S. Turquety
LMD, Laboratoire de Météorologie Dynamique, UMR CNRS 8539, Ecole Polytechnique, Ecole Normale Supérieure, Université P. M. Curie, Ecole Nationale des Ponts et Chaussées, Palaiseau, France
G. Rea
LMD, Laboratoire de Météorologie Dynamique, UMR CNRS 8539, Ecole Polytechnique, Ecole Normale Supérieure, Université P. M. Curie, Ecole Nationale des Ponts et Chaussées, Palaiseau, France
R. Briant
LMD, Laboratoire de Météorologie Dynamique, UMR CNRS 8539, Ecole Polytechnique, Ecole Normale Supérieure, Université P. M. Curie, Ecole Nationale des Ponts et Chaussées, Palaiseau, France
M. Mallet
Laboratoire d'Aérologie, UMR CNRS 5560, Université P. Sabatier, Toulouse, France
J. Sciare
LSCE, Laboratoire des Sciences du Climat et de l'Environnement, UMR CNRS 8212, CEA, Université Versailles St Quentin, Gif sur Yvette, France
LISA, Laboratoire Inter-Universitaire des Systèmes Atmosphériques, UMR CNRS 7583, Université Paris Est Créteil et Université Paris Diderot, Institut Pierre Simon Laplace, Créteil, France