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Knowledge of raindrop size distribution (RSD) is essential for understanding microphysical processes occurring within cloud and precipitation systems, as well as for enhancing the capabilities of numerical models and radar-based quantitative precipitation estimation (QPE). However, observation and study of RSD, especially its temporal and spatial variability, remain quite limited in specific regions. One such region is Southeast China. In this paper, four years of disdrometer data from a south coastal plain site (CPS) and a north hilly inland site (HIS) in the Fujian Province of Southeast China are analyzed and compared to elucidate the characteristics and discrepancies of RSD between these two distinct climatological sites. On this basis, empirical relations between the parameters of Gamma distribution and between radar reflectivity factor (Z) and rain rate (R) are proposed. The results are summarized as follows. (1) In the cases of light to moderate rains, HIS exhibits a higher (lower) concentration of small-size (midsize and large) raindrops with diameters of D < 1 mm (1
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