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《Acta Meteorologica Sinica》 1958-02
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KAO YU-HSIE (Institute of Geophysics and Meteorology,Academia Sinica)  
In this paper,the well-known phenomena of the so-called high autumnclear weather in China is defined and the regions where it most frequentlyoccurs are also determined.After analyzing the variation of 5-days meanrainfall patterns,the dates of its onset and ending are then given.Mean-while,it is pointed out that these dates are also the dates of beginning ofwinter monsoon or retreatment of summer monsoon in the surface layer andonset of westerly jet-stream over SE—Asia or ending of the influence of sum-mer monsoon in upper level respectively.Besides,in comparison the saidweather with the Indian-summer in North America and old-women weather inEurope,it is found that there are some dissimilarities among them,especiallythe difference in the formation factors.
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