Influences of vertical transport and scavenging on aerosol particle surface area and radon decay product concentrations at the Jungfraujoch (3454 m above sea level)

Concentrations of the aerosol particle surface area ( S A ) and aerosol‐attached radon decay products 214 Pb and 212 Pb have been measured by means of an aerosol and a radon epiphaniometer at the Jungfraujoch research station (JFJ; 3454 m above sea level, Switzerland). These parameters exhibit a pronounced seasonal cycle with minimum values in winter and maximum values in summer. In summer, pronounced diurnal variations with a maximum at 1800 LST are often present. Highest concentrations and most pronounced diurnal variations occur during anticyclonic weather conditions in summer. Thermally driven vertical transport over alpine topography is responsible for this observation. During this synoptic condition, concentrations vary greatly with the 500 hPa wind direction, exhibiting low concentrations for NW‐N winds and high concentrations for weak or S‐SW winds. Lead‐214 and S A are highly correlated during anticyclonic conditions, indicating transport equivalence of the gaseous 214 Pb precursor, 222 Rn, and of aerosol particles. When cyclonic lifting is the dominant vertical transport, wet scavenging of aerosol particles can explain the weak correlation of 214 Pb and S A . This conclusion is corroborated by the 214 Pb/ S A ratio, being twice as high during cyclonic than during anticyclonic conditions. Lead‐212 is a tracer for the influence of surface contact on a local scale due to its short lifetime of 15.35 hours. The analysis of this parameter suggests that high‐alpine surfaces play an important role in thermally driven transport to the JFJ.