Cloudbursts occur due to the rapid condensation of moisture-laden air, often triggered by orographic lifting in mountainous areas. As moist air is forced upward by the terrain, it cools and condenses rapidly, leading to intense rainfall. The variability in topography and regional atmospheric conditions in the IHR contributes to the frequency and intensity of these events. Understanding the relationship between physical and thermodynamical atmospheric parameters is crucial for predicting cloudbursts.