中文摘要：

在中国上的台风降水的时间空间的特征在这研究被分析。结果证明台风降水盖住大多数中央东方的中国。台风降水逐渐地从东南的沿海的区域减少到西北的大陆。当最小的年度台风降水内部蒙古，山西， Shaanxi 和四川部分地发生时，最大的年度台风降水在海南的中央东方的台湾和部分超过 700 公里，与价值不到 10 公里。通常，台风在 4 月期间在中国上生产降水 - 有在 8 月的一座山峰的 12 月。为观察车站的年度台风降水时间系列为长期的趋势被检验。结果证明减少的趋势从 1957 ～ 2004 在大多数车站存在并且台湾，海南，沿海的东南中国和南部的东北部分地是统计上重要的中国。台风降水的异例主要在赤道的中央、东方的太平洋上在亚洲和行人房间发行量上源于一般发行量的。台风奔流的雨是在中央大陆的东南的沿海的区域和部分的极端降雨事件之一。在这些区域，奔流的雨被台风主要引起。

英文摘要：

The spatio-temporal characteristics of typhoon precipitation over China are analyzed in this study. The results show that typhoon precipitation covers most of central-eastern China. Typhoon precipitation gradually decreases from the southeastern coastal regions to the northwestern mainland. The maximum annual typhoon precipitation exceeds 700 mm in central-eastern Taiwan and part of Hainan, while the minimum annual typhoon precipitation occurs in parts of Inner Mongolia, Shanxi, Shaanxi and Sichuan, with values less than 10 mm. Generally, typhoons produce precipitation over China during April - December with a peak in August. The annual typhoon precipitation time series for observation stations are examined for long-term trends. The results show that decreasing trends exist in most of the stations from 1957 to 2004 and are statistically significant in parts of Taiwan, Hainan, coastal Southeast China and southern Northeast China. The anomaly of typhoon precipitation mainly results from that of the general circulation over Asia and the Walker Cell circulation over the equatorial central and eastern Pacific. Typhoon torrential rain is one of the extreme rainfall events in the southeastern coastal regions and parts of central mainland. In these regions, torrential rains are mostly caused by typhoons.