Single particle characteristics and ice nucleation potential of particles collected during Asian dust storms in 2021.

ABSTRACT

Dust storms have great impacts on air quality and climate. Dust can influence cloud microphysical properties and determine their radiative forcing and precipitation. Asian dust storms (ADS) are important sources of global aerosol. However, the physiochemical characteristics of dust from ADS at a single particle level are less understood, and the exact particles that can serve as ice nucleating particles (INPs) remain unclear. Here, we present the physicochemical properties and ice nucleation ability of dust particles collected in Beijing during two major ADS in March 2021. The particles from two ADS were classified into Illite, Kaolinite, Feldspar, Quartz, Chlorite, Mixed-dust, and Non-dust particles, which contributed 28.6 % ±â€¯3.3 %, 20.0 % ±â€¯3.9 %, 12.3 % ±â€¯2.3 %, 11.1 % ±â€¯2.8 %, 9.8 % ±â€¯0.8 %, 13.7 % ±â€¯1.8 %, and 4.4 % ±â€¯1.7 % in number, respectively. On average, the ADS particles formed ice crystals via deposition ice nucleation from relative humidity with respect to ice (RHice) of 112 % ±â€¯1 % at 250 K to 154 % ±â€¯15 % RHice at 205 K. Part of the samples also formed ice via immersion freezing between 230 K and 250 K. Among the 149 identified INPs, Clay-like particles (Chlorite, Illite, and Kaolinite) contributed 71.1 % ±â€¯6.2 % in number and followed by Mixed-dust-like particles (16.9 % ±â€¯8.7 %) and Feldspar-like particles (10.4 % ±â€¯6.3 %). Enrichment factor for each particle type is calculated as the ratio of its number fractions in INPs and the aerosol population. It ranges from 0.6 ±â€¯0.7 to 1.3 ±â€¯2.2. The contribution of each particle type to INP was correlated with its fraction in the population. These results imply that each particle type can serve as INP. Clay-like particles are the dominant INPs during the ADS. We conducted ice nucleation kinetic analysis and provided parameterizations of heterogeneous ice nucleation rate coefficient and contact angle for ADS. These parameterizations can be used in the modeling study to evaluate the impact of ADS in atmospheric ice crystal formation in clouds.