Abstract:By using on-site survey data, combined with Doppler weather radar, automatic weather station, and lightning data, the wind type and wind intensity of wind damage occurred in Baoying County on June 29, 2019 were analyzed. The results show that: (1) the objects damaged by the strong wind were distributed in the same direction, with no sign of wind convergence, and the fragment scattering range was small, which was consistent with the distribution characteristics of linear thunderstorm gale features. Judging from the distribution of tile fragments and the direction of the broken trees, the wind direction of the ground strong wind was southwest or south. When the wind damage occurred, the highest intensity of gusts was about violent storms according to the EF grade standard. (2) At 02:00 BST of June 29, the surface cyclone moved northward from Jinhu to Baoying. Due to the pressure gradient force, a rotating wind with a maximum wind speed of 4—6 grade was generated in the vicinity of the low-pressure center. The maximal wind was located on the south side of the low-pressure center and the wind direction was southwest. The lightning data showed that the lightning activity in Baoying was weak during the time of the wind damage occurred, indicating that the corresponding convective storm intensity was weak and could not generate a tornado. (3) Radar data analysis shows that the convective monomer does not have the super-cell echo structure, and the radial velocity map does not recognize the medium cyclone and TVS. The radial velocity showed that a jet stream appeared in the middle layer, and the strong divergent airflow was superimposed on the southwest wind on the south side of the cyclone center, which increased the surface wind speed. Therefore, the wind damage was caused by the strong wind formed by the superposition of the sinking and outflow caused by the convective storm southwest wind and the Barometric gradient wind caused by the cyclone.