Aerosol-cloud interactions have a significant effect on the energy budget of the summertime high Arctic (north of 80°). During the sunlit summer months, low clouds have a net warming effect on the atmospheric boundary layer (Tjernström et al., 2012). In cloud-free conditions, surface air temperatures are typically lower by several degrees. Isentropic atmospheric transport to the summertime high Arctic is limited by "domes" of low constant potential temperature, particularly at lower elevations (Klonecki et al., 2003;Stohl, 2006). In fog-forming and cloud-forming conditions, northward air transport at low levels occurs (