EN ISO 15927-3:2009
Current
The latest, up-to-date edition.
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)
15-03-2009
Foreword
Introduction
1 Scope
2 Terms, definitions, symbols and units
3 Calculation of airfield indices from hourly wind
and rain data
4 Estimation of the effect of driving rain from
average wind and present weather code for rain
5 Calculation of wall indices
Annex A (informative) Limits to the validity of the
calculated indices
Annex B (informative) The nature of a "spell" of driving rain
Annex C (informative) The procedure for generating the
driving-rain maps
Annex D (informative) Comparison of methods specified
in Clauses 3 and 4
Bibliography
ISO 15927-3:2009 specifies two procedures for providing an estimate of the quantity of water likely to impact on a wall of any given orientation. It takes account of topography, local sheltering and the type of building and wall.The first method, based on coincident hourly rainfall and wind data, defines the method of calculation of 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, based on average wind data and a qualitative recording of the presence and intensity of rain (the present weather code for rain), defines a method for calculating the spell length during which an absorbent material such as masonry is moistened, having a 10 % probability of being exceeded in any year (commonly referred to as having a mean return period of 10 years).ISO 15927-3:2009 provides a comparison between the two methods.ISO 15927-3:2009 gives procedures to correct the results of both methods for topography, local sheltering and the type of building and wall.The methods included in ISO 15927-3:2009 do not apply in mountainous areas with sheer cliffs or deep gorges, in areas in which more than 25 % of the annual rainfall comes from severe convective storms, and in areas and during periods when a significant proportion of precipitation is made up of snow or hail.
Committee |
CEN/TC 89
|
DocumentType |
Standard
|
PublisherName |
Comite Europeen de Normalisation
|
Status |
Current
|
Standards | Relationship |
DIN EN ISO 15927-3:2009-08 | Identical |
ISO 15927-3:2009 | Identical |
NS EN ISO 15927-3 : 2009 | Identical |
SN EN ISO 15927-3 : 2009 | Identical |
NEN EN ISO 15927-3 : 2009 | Identical |
I.S. EN ISO 15927-3:2009 | Identical |
NF EN ISO 15927-3 : 2009 | Identical |
BS EN ISO 15927-3:2009 | Identical |
UNI EN ISO 15927-3 : 2009 | Identical |
UNE-EN ISO 15927-3:2011 | Identical |
NBN EN ISO 15927-3 : 2009 | Identical |
PN EN ISO 15927-3 : 2010 | Identical |
04/30124006 DC : DRAFT OCT 2004 | EN 15026 - HYGROTHERMAL PERFORMANCE OF BUILDING COMPONENTS AND BUILDING ELEMENTS - ASSESSMENT OF MOISTURE TRANSFER BY NUMERICAL SIMULATION |
VDI 4710 Blatt 4:2015-09 | Meteorological data for the building services - t,x correlations and wind statistics for 122 European cities |
VDI 4710 Blatt 1:2013-03 | Meteorological data for building-services purposes - Non-European climatic data |
BS 8104:1992 | Code of practice for assessing exposure of walls to wind-driven rain |
VDI 3786 Blatt 2:2000-12 | Environmental meteorology - Meteorological measurements concerning questions of air pollution - Wind |
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