Abstract:Based on the GMS Infrared radiation TBB,NCEP 1°x 1°reanalysis data,T-lnP and rainfall data of surface automatic stations,a MCC weather process occurred in mid-south of Hebei province on June 27,2008 was diagnosed.Results showed that from the forming stage to the mature period of the MCC,severe convective weather such as thunderstorms,heavy precipitation,gales appeared in west of the MCC where the TBB grads was biggest.The main weather systems caused the MCC were upper vortex,the trough in the upper layer and the ground wind shear.The environmental conditions of high temperature and humidity in the lower troposphere provided a favorable thermodynamic condition for the forming and developing of MCC.The low level jet of 850 hPa provided abandant vapor for the heavy rain,which occurred in the overlapping zone of negative MPV1 and positive MPV2.