Abstract:The reanalysis data of NCEP FNL 0.25°×0.25° and the precipitation data of Zhejiang mesoscale meteorological stations are used for the diagnostic analysis on "Lekima" rainstorm. The results are as follows:(1) Heavy rainfall is mainly in the southwest part of the near typhoon center and the north part, which is slightly far from it, with the eye wall precipitation near the typhoon center and the spiral cloud belt precipitation in the north part. (2) The large-value area of the 850 hPa to 925 hPa water vapor flux convergence is consistent with the actual heavy rainfall area, and the difference in intensity of water vapor convergence is the key to the difference in the areas of the heavy typhoon eye wall precipitation. (3) The uplifting movement of the system near the typhoon center is strong while the typhoon is strong, the decrease of the central value of the positive helicity and the decrease of the center correspond to the occurrence of heavy precipitation, and the overlap between the low-level positive vertical helicity and the high-level negative vertical helicity center has certain indications to the convective precipitation. (4)The region with the most obvious topographic gain in this process is in the northern part of Taizhou, and the precipitation sub-centers appears even when the water vapor conditions are at a disadvantage.