| description abstract | In summer, the complex layout of the coasts and mountains surrounding the western Mediterranean basin favors the development of mesoscale atmospheric recirculations and the formation of ozone reservoir layers above the coastal areas and the sea. Tropospheric ozone cycles vary here according to location and exposure of the monitoring station in relation to the flows and reservoir layers, and large differences can be encountered within tens of kilometers. The basic premise for this work is that the representativeness of any station is determined by the (fore)knowledge of the processes affecting the site, at the proper timescales and space scales within its region. Thus, available data have been combined with mesoscale analysis and modeling to interpret the observed summer ozone cycles for the monitoring network at Castellón, on the Spanish east coast. The area is approximately 120 km by 120 km, is backed by coastal mountains, and includes the following: a conurbation, industries, and a densely traveled road network parallel to the coast. To summarize the results, a typology has been developed that relates the variability in the observed ozone cycles to the site locations, the documented mesoscale circulations, and the chemical reactions along the atmospheric paths. Five types have been found to represent the cycles observed in this region, and information available to the authors indicates that this typology covers most nonurban monitoring stations around the western Mediterranean basin. | |
