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1988年7月下旬塔克拉玛干沙漠腹地满西异井测站出现了一次强降水天气，日降水量达28．6mm，证实了在大尺度环流背景下，中小尺度天气系统的影响及午后局地对流发展旺盛时，沙漠腹地同样也能出现强度较大的降水天气。
In late July 1988, a heavy precipitation event occurred at Manxi Xinyu Station in the hinterland of the Taklamakan Desert with a daily precipitation of 28.6 mm, confirming the impact of the meso-scale weather system and the development of local convection in the afternoon under the background of large-scale circulation Exuberant, the hinterland of the desert can also occur with greater intensity of precipitation weather.