Cirrus clouds play an important role in Earth's energy budget by reflecting the incoming solar radiation into space which leads to cooling, and by reducing the infrared longwave coming from the Earth surface which leads to warming (Chen et al., 2000;Heymsfield et al., 2017;Storelvmo & Herger, 2014). The radiative properties of cirrus clouds depend on the ice crystal number concentration, which in turn depends on the aerosol that nucleate ice at these conditions. Cirrus cloud ice crystals form either through homogeneous processes, requiring no ice nucleating particle (INP) or active site, or heterogeneously where an INP is involved (Hoose & Möhler, 2012;Kanji et al., 2017;Vali et al., 2015). Heterogeneous ice nucleation (IN) can occur via deposition of ice on particle surfaces, condensation in pores and subsequent freezing (Campbell et al., 2017;David et al., 2019;Marcolli, 2014), through immersion freezing of droplets as they cool, or condensation freezing as particles simultaneously uptake water and cool. Another freezing path is contact freezing where a particle approaches the air-water interface from either the outside of the droplet or from inside of the droplet (Durant & Shaw, 2005;Kanji et al., 2017). Homogeneous freezing of liquid aerosol is predominantly controlled by water activity (or ambient relative humidity (RH)), temperature, particle size, and hygroscopicity (Baumgartner et al., 2022;Koop et al., 2000;Schneider et al., 2021). Among these, temperature and RH dominate. Chemical composition influences homogeneous IN by modulating hygroscopicity (Junge, 1953;M. D. Petters & Kreidenweis, 2007). However, the overall influence of chemical composition on homogeneous freezing nucleation is small (Kreidenweis et al., 2009). In contrast, heterogeneous IN strongly depends on the chemical composition and morphology (Hiranuma et al., 2014). Ambient measurements of cirrus ice crystal residuals show a wide range of chemical composition, including organic particles, black carbon, mineral dust, lead and other metal bearing particles, sulfate particles, and salt particles