Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder

Building in cold climate zones requires a high insulation thickness and a good protection against interstitional condensation. Applying vapour tight membranes on both sides of a roof construction offers no drying potential in case of leakages or initial moisture. Therefore the use of slightly permea...

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Bibliographic Details
Main Authors: Bludau, C., Künzel, H.M.
Format: Conference Object
Language:English
Published: 2009
Subjects:
690
Online Access:https://publica.fraunhofer.de/handle/publica/362082
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spelling ftfrauneprints:oai:publica.fraunhofer.de:publica/362082 2023-05-15T15:08:18+02:00 Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder Bludau, C. Künzel, H.M. 2009 https://publica.fraunhofer.de/handle/publica/362082 en eng International Conference on Cold Climate, Heating, Ventilating and Air-Conditioning 2009 https://publica.fraunhofer.de/handle/publica/362082 690 presentation 2009 ftfrauneprints 2022-11-01T20:04:07Z Building in cold climate zones requires a high insulation thickness and a good protection against interstitional condensation. Applying vapour tight membranes on both sides of a roof construction offers no drying potential in case of leakages or initial moisture. Therefore the use of slightly permeable membranes at the interior side is often preferred because they allow condensed or existent moisture to dry out. However, drying to the interior space will only happen if the solar heat gains of the roof are high enough to inverse the vapour flow for a sufficient time period. This paper looks to the climate limits of building flat roofs with moderately permeable vapour retarders. The balance of interstitial condensation and subsequent drying is investigated using an adapted hygrothermal simulation tool for heat and moisture transport in building components. For the simulations a black surfaced flat roof construction with mineral fibre insulation and moderate vapour retarder is considered. Special interest is set on the drying potential in relation to the building's location in Northern climate zones. The results can be shown by two limit lines around the North Pole, one for vapour retarders with a constant permeability and the other for those with humidity controlled permeability. These lines are not parallel to the Arctic Circle. They reflect the regional climate conditions which are influenced by the Gulf Stream and other meteorological phenomena. Conference Object Arctic North Pole Publikationsdatenbank der Fraunhofer-Gesellschaft Arctic North Pole
institution Open Polar
collection Publikationsdatenbank der Fraunhofer-Gesellschaft
op_collection_id ftfrauneprints
language English
topic 690
spellingShingle 690
Bludau, C.
Künzel, H.M.
Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
topic_facet 690
description Building in cold climate zones requires a high insulation thickness and a good protection against interstitional condensation. Applying vapour tight membranes on both sides of a roof construction offers no drying potential in case of leakages or initial moisture. Therefore the use of slightly permeable membranes at the interior side is often preferred because they allow condensed or existent moisture to dry out. However, drying to the interior space will only happen if the solar heat gains of the roof are high enough to inverse the vapour flow for a sufficient time period. This paper looks to the climate limits of building flat roofs with moderately permeable vapour retarders. The balance of interstitial condensation and subsequent drying is investigated using an adapted hygrothermal simulation tool for heat and moisture transport in building components. For the simulations a black surfaced flat roof construction with mineral fibre insulation and moderate vapour retarder is considered. Special interest is set on the drying potential in relation to the building's location in Northern climate zones. The results can be shown by two limit lines around the North Pole, one for vapour retarders with a constant permeability and the other for those with humidity controlled permeability. These lines are not parallel to the Arctic Circle. They reflect the regional climate conditions which are influenced by the Gulf Stream and other meteorological phenomena.
format Conference Object
author Bludau, C.
Künzel, H.M.
author_facet Bludau, C.
Künzel, H.M.
author_sort Bludau, C.
title Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
title_short Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
title_full Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
title_fullStr Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
title_full_unstemmed Flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
title_sort flat roofs in cold climates - climatic limits for building flat roofs with a permeable vapor retarder
publishDate 2009
url https://publica.fraunhofer.de/handle/publica/362082
geographic Arctic
North Pole
geographic_facet Arctic
North Pole
genre Arctic
North Pole
genre_facet Arctic
North Pole
op_relation International Conference on Cold Climate, Heating, Ventilating and Air-Conditioning 2009
https://publica.fraunhofer.de/handle/publica/362082
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