The Influence of Secondary Ice Crystal Release on the Electrical Structure of Convective Clouds and the Quality of Thunderstorm Forecasting
摘要
This study enhances thunderstorm prediction accuracy by integrating the Hallett-Mossop (HM) secondary ice production mechanism into a coupled Weather Research and Forecasting (WRF-ARW) model with an electrification module. The WRF-ARW model was configured with a 2 km convection-permitting grid and the Thompson-Eidhammer two-moment microphysics scheme, explicitly resolving deep convective updrafts over Central Russia during the 2021 convective season (May 15–August 31). The HM mechanism, active at temperatures between −8 °C and −3 °C, increases ice crystal number concentration (m−3), amplifying volume charge density (nC/m3) via collisional fragmentation. Validated against multi-source lightning data (WWLLN, TLN, MGO, VGI), the HM-enhanced model outperforms traditional non-inductive/inductive schemes, increasing thunderstorm detection accuracy (Probability of Detection) by 16% and reducing false alarms by 13%. Coupling HM with the Tiedtke (Monthly Weather Review 117(8): 1779–1800, 1989) convection parameterization at 6 km resolution confirms robustness, but the 2 km configuration achieves the highest skill scores (Gilbert criterion = 59%, Bagrov-Heidke criterion = 0.39). This framework advances short-term thunderstorm forecasts, with applications in aviation safety, energy infrastructure protection, and disaster preparedness.