2; power spectral density"/> 2 are good indicators to reflect the beginning and termination of a rainfall process. For rain events, radial velocity is positive, spectral width broadens in power spectral density diagrams, and the shapes of all signals are similar. (3) Velocity ambiguity in radial velocity maps denotes severe weather processes. Strong wind is happening if velocity ambiguity is at a low level. The wind profiler radar is a reliable instrument to predict the occurrence and development of severe convective weather. The local short-term and nowcasting capability can be effectively strengthened with the Doppler radar data."/>
Archive > Volume 50 Issue 3 > 2022,50(3):369-379. DOI:10.19517/j.1671-6345.20210006 Prev Next

Application of Boundary Wind Profile Radar to Severe Convective Weather Forecast in Central Zhejiang

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