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《Meteorological Monthly》 2007-08
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Mechanism Analysis of Rainfall in the Far Distance of Typhoon AERE

Fan Xuefeng1,2 Wu Zhen2 Xi Shiping2(1.College of Atmospheric Sciences,Lanzhou University,730000;2.Henan Meteorological Observatory)  
By using the helicity and moist potential vorticity(MPV)theory 1°×1° reanalysis data of NCEP was calculated to diagnose the heavy rain process of NO.18 Typhoon AERE in the east of Henan.The dynamical and thermodynamic mechanisms of this process' formation and development were discussed.The results show that southeast jet in the typhoon inverted trough periphery supplied vapor and thermodynamic conditions for the heavy rain.Strong convergence action on the top of typhoon inverted trough was the dynamical mechanism of the rainstorm' happening and developing.Because of weak cool air intrusion in the low level the MPV1 of rainstorm area turned from negative to positive,which led vertical vortexes to enhance and hasten precipitation developing.So the weak cool air intrusion increased the precipitation in some extent.Moreover,the moving and developing of big value band of the vertical helicity of 925hPa could dictate the place of inverted trough and had better indicative meaning for rainstorm falling area.When the rainstorm happened the area was in the negative big value area of MPV1.
【CateGory Index】: P458.124
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