摘要
Based on conventional data from automatic stations in Shanghai City,data of temperature of black body(TBB) obtained by Japan MTSAT satellite,Doppler radar data of Nantong,and 1.0°× 1.0° NCEP reanalysis data,the development characteristics and triggering mechanisms of a mesoscale thunderstorm process in Shanghai on June 23,2013 were analyzed. The results show that the thunderstorm process was triggered by flow fields at high and low altitudes and the transport of sufficient water vapor at low altitudes.
Based on conventional data from automatic stations in Shanghai City,data of temperature of black body(TBB) obtained by Japan MTSAT satellite,Doppler radar data of Nantong,and 1.0° × 1.0° NCEP reanalysis data,the development characteristics and triggering mechanisms of a mesoscale thunderstorm process in Shanghai on June 23,2013 were analyzed. The results show that the thunderstorm process was triggered by flow fields at high and low altitudes and the transport of sufficient water vapor at low altitudes.
