Numerical Simulation of a Hail Event Form Mechanism in Shenyang, Liaoning Province
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Abstract:
The meso-scale strong convection weather system is successfully simulated with a meso-scale numerical model, that leads to a hail weather in Shenyang on June the 28th in 2003.Combining intensive observations, convertional data and model output products, the meso-scale synoptic system is analyzed particularly. The diagnosis is done. The mechanism of Shenyang hail is discussed.