3).

Saharan dust outbreaks and iberulites

The general content of aerosols in the atmosphere of the southern Iberian Peninsula is clearly related to the evolution of aerosols arriving from North Africa. Monitoring of dry aerosol deposition using passive samplers determined the formation of iberulites in two periods of the year (Fig. 4). The main depositional period occurs throughout the summer, while the second appears as a minor peak in early spring. However, the formation of iberulites is more specifically related with Saharan

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