Application of Surface Automatic Meteorological Station Datato Detecting Rainstorm Processes
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Abstract:
The distribution of the surface elements of two rainstorm processes is analyzed during 6-7 and 9-10, July 2005 by using the surface automatic meteorological station data and satellite data. It shows that the strong rainfall belt lies near the nonfrontal baroclinic zone and baroclinic troughs. Using the NECP data, the dynamic mechanis of the nonfrontal baroclinic zone and baroclinic troughs causing strong precipitation are revealed by the thermal wind helicity of the second kind and the ageostrophic wet Qvector, it indicates that frontogenesis and baroclinic zone easily occur in the surface nonfrontal baroclinic zone and baroclinic troughs, and then they may induce the strong precipitation.