Based on the instability conditions, FY-2E satellite images and Doppler radar data, a severe convective weather accompanied by gust front which occurred on August 23, 2015 in Guanzhong of Shaanxi was analyzed. The results indicated that this process belongs in fore-trough dry convection although it took place in front of trough, while the humidity of high-altitude was less than that of the low-altitude. 850 hPa shear line provided initial disturbance for the strong convection which was triggered by ground convergence line. Two gust fronts both appeared at the edge of convective clouds where the gradient of TBB reached a maximum with severe release of CAPE. Opposite movement of two gust fronts caused the engendering of strong convective cells. With the superimposition of strong convective clouds and gust front, both of them weakened each other, which caused disappearance of gust front. On the other hand, convective clouds grew fast because of supplement of new convective cells, which led to stronger convective weather.
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