<![CDATA[This study investigates the microphysical and dynamical characteristics of hail-producing convective clouds over the Depok region, Indonesia, through a case study of the event on 28 October 2024. A multi-data approach was applied by integrating weather radar data, Himawari-9 satellite, and ERA5 atmospheric reanalysis. Radar analysis revealed intense convective cores with reflectivity exceeding 55–60 dBZ, high Vertically Integrated Liquid (VIL) values (~50 mm), and ZHAIL probabilities above 80%, indicating well-developed hail cores. Satellite observations showed cloud growth and extremely low cloud-top temperatures coinciding with peak radar signatures. Although Convective Available Potential Energy (CAPE) values were relatively modest, reanalysis data indicated strong moisture availability, deep-layer instability, and favorable wind shear. These results demonstrate that hail formation in tropical urban regions is driven by the combined effects of moisture-rich environments, deep atmospheric instability, and organized convective dynamics rather than by high CAPE alone.]]>
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