A comparison of the concentrations of IN at three different altitudes showed (refer the supplementary file for more detailed information) that the concentration of IN at the foot of the mountains was higher than that at the summit, indicating that more aerosols near the ground cause high concentrations of IN. Further analysis of the source of atmospheric ice nuclei found that high correlation between IN and aerosol particles with size larger than 0.5μm, indicating that the large aerosol particles contribute more to IN. Through the comparison with the IN measurements obtained in three different regions, it is found that the number concentration of IN in Nanjing is the highest, followed by that in Xinjiang (no–dust days), and the lowest on Mts. Huangshan. As for the proportionality of IN number concentration to aerosol particle concentration, it is the highest in Xinjiang and the lowest on Mts. Huangshan.
In addition, parameterizations were developed based on measurements to represent the variations of IN concentration with temperature, supersaturation, and the number concentration of aerosol particles with size larger than 0.5μm. They can be applied to the surface of the desert, the relatively clean background areas and the polluted city regions.