Abstract. In the framework of ChArMEx (the Chemistry-Aerosol Mediterranean
Experiment), the air quality model Polyphemus is used to understand the
sources of inorganic and organic particles in the western Mediterranean and evaluate the uncertainties linked to the model parameters (meteorological
fields, anthropogenic and sea-salt emissions and hypotheses related to the model
representation of condensation/evaporation). The model is evaluated by
comparisons to in situ aerosol measurements performed during three
consecutive summers (2012, 2013 and 2014). The model-to-measurement
comparisons concern the concentrations of PM10, PM1, organic matter
in PM1 (OM1) and inorganic aerosol concentrations monitored at a
remote site (Ersa) on Corsica Island, as well as airborne measurements
performed above the western Mediterranean Sea. Organic particles are mostly
from biogenic origin. The model parameterization of sea-salt emissions has
been shown to strongly influence the concentrations of all particulate species
(PM10, PM1, OM1 and inorganic concentrations). Although the
emission of organic matter by the sea has been shown to be low, organic
concentrations are influenced by sea-salt emissions; this is owing to the fact that they provide a
mass onto which gaseous hydrophilic organic compounds can condense. PM10,
PM1, OM1 are also very sensitive to meteorology, which affects
not only the transport of pollutants but also natural emissions (biogenic
and sea salt). To avoid large and unrealistic sea-salt concentrations, a
parameterization with an adequate wind speed power law is chosen. Sulfate is
shown to be strongly influenced by anthropogenic (ship) emissions. PM10,
PM1, OM1 and sulfate concentrations are better described using the
emission inventory with the best spatial description of ship emissions
(EDGAR-HTAP). However, this is not true for nitrate, ammonium and chloride
concentrations, which are very dependent on the hypotheses used in the model
regarding condensation/evaporation. Model simulations show that sea-salt aerosols
above the sea are not mixed with background transported aerosols. Taking
the mixing state of particles with a dynamic approach to condensation/evaporation into
account may be necessary to accurately represent inorganic
aerosol concentrations.