中文摘要：

从在福建省的台风降水从 5 月发生到 11 月的 1960 ～ 2005 表演影响福建的台风降水的时间、空间的分发的分析的结果，与在 8 月的大多数。自从 1960，有一个减少的趋势。台风降水逐渐地从沿海的区域减少到福建的西北的大陆，最大的台风降水发生在东北和福建的南方。台风奔流的雨是在福建的极端降雨事件之一。台风的高频率奔流的雨发生在沿海并且省的西南区域。与福建的地面的影响，台风降水比到西方更容易发生到山的东方。在在赤道的东方太平洋的亚洲和海表面温度异例上的 500 hPa 的大气的循环被分析，与发现他们仔细与影响福建的台风 降水的异例被连接，可能主要由 modulating 经由改变空气发行量在省上导致台风 降水的异例的台风的向北行的轨道

英文摘要：

The results of an analysis of the temporal and spatial distribution of typhoon precipitation influencing Fujian from 1960 to 2005 show that typhoon precipitation in Fujian province occurs from May to November, with the most in August. There has been a decreasing trend since 1960. Typhoon precipitation gradually decreases from the coastal region to the northwestern mainland of Fujian and the maximum typhoon precipitation occurs in the northeast and the south of Fujian. Typhoon torrential rain is one of the extreme rainfall events in Fujian. High frequencies of typhoon torrential rain occur in the coastal and southwest regions of the province. With the impact of Fujian＇s terrain, typhoon precipitation occurs more easily to the east of the mountains than to the west. Atmospheric circulation at 500 hPa over Asia and sea surface temperature anomalies of the equatorial eastern Pacific are analyzed, with the finding that they are closely connected with the anomaly of typhoon precipitation influencing Fujian, possibly mainly by modulating the northbound track of typhoons via changing the atmosphere circulation to lead to the anomaly of typhoon precipitation over the province