Understanding the impact of aerosols on heavy precipitation is crucial for improving predictions and management of atmospheric processes. Heavy convective precipitation often occurs within a few hours, making the investigation of aerosol influences on daily precipitation variability particularly important. In this study, heavy rainfall events in southwestern Iran were identified using ERA5 data alongside aerosol measurements from two satellite sources and the EAC4 reanalysis dataset. These datasets enabled analysis of aerosol optical depth (AOD), differentiation of aerosol types, and assessment of additional aerosol-related indices in the region. Two indices were used to classify clean and polluted conditions at macro- and micro-scales: AOD as a large-scale indicator, and cloud droplet number concentration (CDNC) as a small-scale indicator. The 25th and 75th percentiles of these indices over all rainy days were used as thresholds for clean and polluted conditions. Four aerosol types common in southwestern Iran were examined: black carbon (BC) and dust as radiatively absorbing aerosols, and sulfate and sea salt as non-absorbing aerosols. Analysis revealed three key features of daily heavy precipitation variability associated with aerosol types. Under polluted conditions defined by AOD, precipitation onset and peak occurred earlier, but event duration was shorter. In contrast, under polluted conditions defined by CDNC, precipitation started earlier but peaked later, with a longer duration. Furthermore, absorbing aerosols were associated with earlier onset and delayed peaks, whereas non-absorbing aerosols corresponded to delayed onset and extended precipitation duration. These findings highlight the distinct roles of aerosol types in modulating heavy rainfall characteristics.
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