Spatial variation of the aerosol concentration and deposition over the
Mediterranean coastal zone
J. Piazzola ⁎, G. Tedeschi, R. Blot
LSEET, Southern University of Toulon-Var, France
article info abstract
Article history:
Received 4 November 2009
Received in revised form 26 March 2010
Accepted 9 April 2010
A model for the spatial variation of aerosol concentrations and deposition along the coastal
zone is of great interest for studies on air and water quality. In coastal areas, sea-spray aerosols
generated at the sea surface by the interaction between wind and waves add to a continental
contribution emitted from natural and/or anthropogenic sources. To include coastal effects in
the model for the prediction of aerosol concentrations, Piazzola et al. (2003) developed the
coastal Mediterranean aerosol model. The present paper deals with an extension of the
Mediterranean coastal aerosol to a regional scale applied to the prediction of the sea surface
flux deposition. This was achieved by the development of an automatic coupling process
between the aerosol model and a regional meso-scale meteorological model which allows
accounting for the details of the orography of the coast. The results show a non-homogeneous
spatial coverage of aerosol concentrations over the northwestern Mediterranean. The
simulations were then validated using aerosol size distributions recorded on board the ship
“Atalante” for two kinds of meteorological conditions. Error calculations show a good
performance of the coupling process since it predicts the aerosol concentration to within a
maximum factor of 3 for particle radii between 0.1 to 10 μm. This process was then used to
provide the spatial distribution of the particle deposition fluxes over the study area.
© 2010 Elsevier B.V. All rights reserved.
Keywords:
Coastal aerosols
Atmospheric models
Deposition
Fetch
1. Introduction
Aerosols particles affect climate by scattering and absorbing
radiation (Charlson et al., 1992), and may affect the heat budget.
Among them, the particles generated at the air–sea interface by
wave breaking represent a major component of the natural
aerosol (Andreae, 1995). Seasalts dominate atmospheric depo-
sition in maritime regions (Gustafsson and Franzen, 1996;
Farrell, 1995). In coastal zones, however, sea spray aerosols
punctually generated at the sea surface are added to a
continental contribution issued from natural and/or anthropo-
genic sources (Mulcahy et al., 2008; Callaghan et al., 2008). In
particular, the Mediterranean Sea is a quite closed sea
surrounded by specific microclimatologic zones. The aerosol
mixture in coastal zones is strongly related to the changes in the
wind direction that could be in turn accompanied by variations
in meteorological parameters. To include coastal effects in the
aerosol model for the prediction of aerosol concentrations,
Piazzola et al. (2003) proposed the coastal Mediterranean
aerosol model (MEDEX) based on an extensive series of
measurements on the island of Porquerolles (off the French
Mediterranean coast, located at about 5 km from the coastline).
The main inputs of the coastal Mediterranean aerosol model are
both the wind speed and the fetch, i.e., the water trajectory of the
wind. The fetch actually represents the distance over water for
which the wind has blown without any major change in both the
intensity and direction. This parametric model showed good
performances when comparing to aerosol distributions mea-
sured in different Mediterranean sites (Bendersky et al., 2004;
Piazzola and Kaloshin, 2005). However, the fate of aerosol
particles in the marine atmosphere is largely unknown.
Knowledge on the spatial variation of aerosol concentrations
should be improved for better estimates of the radiative aerosol
Atmospheric Research 97 (2010) 214–228
⁎ Corresponding author.
E-mail address: piazzola@univ-tln.fr (J. Piazzola).
0169-8095/$ – see front matter © 2010 Elsevier B.V. All rights reserved.
doi:10.1016/j.atmosres.2010.04.003
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