Differential characterization of air ions in boreal forest of Finland and megacity of eastern China

Abstract. Air ions play a crucial role in the new particle formation (NPF), which in turn has the potential to influence global intermediate ions and 7–20 nm large ions) at two “flagship” sites: the SMEAR II site in boreal forest of Finland and the SORPES site in megacity of eastern China. Air ion number size distributions (0.8–42 nm) were measured using a Neutral Cluster and Air Ion Spectrometer (NAIS) at these two sites from June 2019 to August 2020. Our study aims to characterize the similarities and differences in ion characteristics and their contributions to NPF between clean forest and polluted urban environments. At both sites, rising temperatures reduced the difference between positive and negative cluster ion climate and air quality. We conducted a comparative analysis of air ions in three size ranges (0.8–2 nm cluster ions, 2–7 nm concentrations, likely due to an increase in ion mean size or enhanced convection and turbulent mixing that diminish the electrode effect. The median cluster ion concentration at SMEAR II (1270 cm⁻³) was approximately six times higher than at SORPES (220 cm⁻³), which was caused by the high coagulation sink in the urban area. The median large ion concentration at SORPES was nearly three times higher (197 cm⁻³) than that at SMEAR II (67 cm⁻³), which is due to higher aerosol concentrations in megacity, since the cluster ions attaching to neutral particles. The cluster ion concentration was negatively associated with the condensation sink (CS) at both sites, with a significantly stronger negative correlation at SORPES, suggesting that CS was a decisive factor in this urban area. The median formation rates of 2 nm and 3 nm ions at SMEAR II (𝐽₂⁻: 0.033 cm⁻³ s^-1, 𝐽₂⁺: 0.041 cm⁻³ s^-1; 𝐽₃⁻: 0.012 cm⁻³ s^-1, 𝐽₃⁺: 0.016 cm⁻³ s^-1) were similar to those at SORPES (𝐽₂⁻: 0.028 cm⁻³ s^-1, 𝐽₂⁺: 0.025 cm⁻³ s^-1; 𝐽₃⁻: 0.028 cm⁻³ s^-1, 𝐽₃⁺: 0.027 cm⁻³ s^-1). The median ion-induced fractions were 19.9 % and 1.3 % at SMEAR II and SORPES, respectively, indicating a minor contribution of ions to NPF in polluted environments. Nevertheless, the charged particles were activated earlier than neutral particles at SORPES, indicating that the ion-induced nucleation could precede neutral nucleation in this polluted environment. In addition, the contribution of ion-induced nucleation at SORPES was higher at low NPF intensity, implying the non-negligible roles of air ions in aerosol production in urban area.