DIN EN ISO 15927-3-2009 建筑物的湿热性能.气候数据的计算和表示.第3部分:根据每小时风雨数据计算垂直表面大雨指数(ISO 15927-3:2009),DIN EN ISO 15

标准号：DIN EN ISO 15927-3-2009
中文标准名称：建筑物的湿热性能.气候数据的计算和表示.第3部分:根据每小时风雨数据计算垂直表面大雨指数(ISO 15927-3:2009),DIN EN ISO 15927-3:2009-08的英文版本
英文标准名称：Hygrothermal performance of buildings - Calculation and presentation of climatic data - Part 3: Calculation of a driving rain index for vertical surfaces from hourly wind and rain data (ISO 15927-3:2009); English version of DIN EN ISO 15927-3:2009-08
标准类型：P31
发布日期：1999/12/31 12:00:00
实施日期：1999/12/31 12:00:00
中国标准分类号：P31
国际标准分类号：91.060.10;91.120.10;91.120.30
适用范围：This part of ISO 15927 specifies two procedures for providing an estimate of the quantity of water likely toimpact on a wall of any given orientation. It takes account of topography, local sheltering and the type ofbuilding and wall.The first method, given in Clause 3 and based on coincident hourly rainfall and wind data, defines a means ofcalculating-- the annual average index, which influences the moisture content of an absorbent surface, such as masonry, and-- the spell index, which influences the likelihood of rain penetration through masonry and joints in other walling systems.The second method, given in Clause 4 and based on average wind data and a qualitative recording of thepresence and intensity of rain (the present weather code for rain), defines a means of calculating the spelllength during which an absorbent material such as masonry is moistened, which has a 10 % probability ofbeing exceeded in any year (commonly referred to as having a mean return period of 10 years).A comparison between the two methods is given in informative Annex D.Procedures are given to correct the results of both methods for topography, local sheltering and the type ofbuilding and wall.The methods included in this part of ISO 15927 do not apply ina) mountainous areas with sheer cliffs or deep gorges,b) areas in which more than 25 % of the annual rainfall comes from severe convective storms,c) areas and periods when a significant proportion of precipitation is made up of snow or hail.