An infrequent continuous rain weather process occurred from September 25 to October 14 in 2007 in northwestChina was studied from theweather and climate background, upper and lower level circulation, surface situation and some physical factors. The results show that frequent activity of thewesterly trough and anomaly of the subtropic high pressure location resulted in this infrequent continuous autumn rain. Moreover, the position ofSouthAsia high at the levelof100 hPa, 500 hPawind field and the position of zero line has some significance for rainfall prediction.