Updating the 1995 national building code of canada wind pressures
This site stores nothing other than an automatically generated session ID in the cookie; no other information is captured.
In general, only the information that you provide, or the choices you make while visiting a web site, can be stored in a cookie.
To provide access without cookies would require the site to create a new session for every page you visit, which slows the system down to an unacceptable level.
The houses are marketed internationally and so must resist tropical cyclone wind loadings.
Two full-scale shelters, measuring 4.9 m×6.1 m in plan, were subjected to static forces equivalent to loads caused by wind acting normal to the ridge of the roof.
There are many reasons why a cookie could not be set correctly.The shelter generally performed well, but was susceptible to premature local failures in regions where tension was applied through the thickness of corrugated fibreboard panels or where the quality of construction was imperfect.The testing apparatus also generally performed well, once its connections to the specimen were modified to eliminate localized areas of high stress and the relatively large deformation of the specimen were accommodated. Updating Wind Pressures for the 1995 National Building Code of Canada. has developed a modular house for emergency, temporary or semi-permanent occupation that uses corrugated fibreboard as the main structural material. Meteorological Service of Canada – Ontario Region, 2001. Graphics Provided Courtesy of Erik Buhler of the Ontario Storm Prediction Centre, Toronto. Reviewed and approved by Canadian Commission on Building and Fire Codes Ottawa. Meteorological Service of Canada, Toronto, Ontario. In the future, more work needs to be done to estimate ice amounts due to other forms of icing such as in-cloud rime icing and wet snow.These quantities should be added to the current amounts to make the ice map complete.Horizontal ice accretion thickness is assumed to be the observed precipitation amount adjusted by the appropriate ice density. Vertical ice accretion thickness is proportional to precipitation rate and wind speed. Horizontal and vertical ice thicknesses are changed into equivalent radial thickness (Chaine and Castonguay, 1974).Ice accretion occurs only at temperatures near or below freezing. All parameters used in this model can be derived from routinely observed meteorological data.