The dry particle size distributions of hybrid flare agents typically had a mode at around 140‐170 nm, being about the same size as that of hygroscopic flare particles. The κ‐value mostly exceeded 0.3, which were comparable to that of typical atmospheric aerosols, and also higher than representative κ‐value of pure mineral dust particles that can be assumed as background aerosol in arid and semi‐arid regions. The large portion of submicron particles was predominantly affected by both potassium chloride and calcium chloride included in individual particles. Those materials have strong hygroscopicities. Additionally, most of hybrid flare particles were also mixed with tiny AgI particles. The number of INP induced per gram of hybrid flare agents measured by IN counter and the derived INAS density at water supersaturation of five percent at temperatures of ‐10, ‐15, ‐20 and ‐25 °C were about 1011‐1013 particles/gram and 1010‐1012 m‐2, respectively. The results also indicated that hybrid flare particles will act as not only immersion freezing nuclei, but also deposition nuclei. The hybrid flare particles eventually act as more effective ice nucleating particles than the atmospheric aerosols in clouds as well as AgI flare particles do. Size dependency of hybrid flare particles’ INP ability has been also studied using size selected particles from hybrid flare. Further investigations of the effects of hybrid flare particles on initial microphysical structures of clouds will be performed using the MRI cloud simulation chamber.