What is it about?
This study consists of a long-term monitoring of Saharan dust outbreaks producing haze that reaches the southern Iberian Peninsula. Aerosol concentration, relative humidity, and temperature time series available at the ground stations in this area indicate sharp variations of these atmospheric variables during the iberulite-forming events. These events mainly occurred during the summer, when it is reached a minimum threshold in the content of large aerosol particles (PM10>15μg×m3).
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Why is it important?
Iberulites are the result of the atmospheric scavenging. Until now was unknown that this scavenging could be the responsible of aggregation phenomena, represented by the iberulites. But this only occurs with specific levels of aerosols.
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This page is a summary of: Saharan dust outbreaks and iberulite episodes, Journal of Geophysical Research Atmospheres, June 2016, American Geophysical Union (AGU),
DOI: 10.1002/2016jd024913.
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