Hygroscopic seeding has been explored in various regions of the world with the goal of enhancing rainfall (Bruintjes, 1999; Flossmann et al., 2019; Silverman, 2003). The conceptual model of hygroscopic seeding focuses on increasing the precipitation efficiency of warm-based convective clouds by broadening the droplet spectra to enhance warm rain formation processes. The approach is to introduce large hygroscopic particles that act as efficient cloud condensation nuclei (CCN) or giant CCN (GCCN), which then nucleate large drops that grow more rapidly via condensation and initiate effective collision-coalescence processes. In addition, this process can suppress the activation of small background aerosols via the "competition effect" (Cooper et al., 1997; Ghan et al., 1998; O'Dowd et al., 1999). Even in mixed-phase, deep convective clouds, the concept suggests that more large drops and drizzle produced from warm rain processes would lead to more active mixed-phase ice formation and subsequent increases in the precipitation efficiency (Lawson et al., 2015; Rosenfeld & Woodley, 1993). Only a few studies have directly measured the broadening of the droplet spectra attributed to hygroscopic seeding (Ghate et al., 2007; Mather et al., 1997). While Rosenfeld et al. (2010) also attempted to directly measure droplet broadening from hygroscopic flare seeding, they were unable to detect a distinct change in the drop size distribution (DSD). However, their observational results were only based upon measurements from one seeded cloud. This study uses data collected in Southeast Queensland to examine the impact of hygroscopic seeding on the initial droplet spectra. A decade-long drought in Southeast Queensland, Australia, in the early 2000s, known as the Millennium Drought (van Dijk et al., 2013) prompted the Queensland government to seek ways to create more water resources, which led to a feasibility study to investigate precipitation enhancement via cloud seeding known as the Queensland Cloud Seeding Research Program (QCSRP; Tessendorf et al., 2010; 2012). Scientists from the United States, South Africa, and Australia conducted the feasibility study, which included a randomized hygroscopic cloud-seeding trial, during the summers in 2007-2009. Given the small number of cases and the high level of natural variability in the QCSRP randomized experiment sample, the results were incomplete and not statistically significant (Tessendorf et al., 2010). This is