Abstract:Using hourly high-altitude and ground conventional observation data, as well as FY-4A satellite products, we analyzed the characteristics of the environmental field and cloud parameter evolution associated with a severe hailstorm in Yan'an. The results show that: (1) The strong convective process was characterized as a cold advection forcing type at high altitude, with the atmospheric stratification described as "dry and cold aloft, warm and humid below", and the ground convergence line triggered instability, leading to widespread thunderstorms. (2) The process was influenced by a highly organized medium-β scale convective system, and the steep drop in TBB values provided an early warning for hail occurrence more than 20 minutes in advance. Hailfall began when the TBB dropped below -32 ℃, and values below -70 ℃ were likely indicative of a hailstorm. (3) The high value area of cloud top height gradient at the front of the mature thunderstorm cloud cluster and the high value area of pressure gradient on the upwind side of the 100 or 200 hPa cloud area correspond to the hail area. The cloud top height exceeding 10 km was an important condition for hailfall onset. (4) The main body of mature thunderstorm cloud was composed of ice clouds. On the upwind side, a transition zone of cirrus, mixed and supercooled water cloudswas observed, and multi-layered cloud structures on the downwind side. (5) The convective initiation product can identify the incipient location of thunderstorm clouds in advance to some extent and predict the enhancement process of these clouds.