Wind Loading of Structures, Third Edition
John D. Holmes
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Wind loading competes with seismic loading as the dominant environmental loading for structures. They have produced roughly equal amounts of damage over a long time period, although large damaging earthquakes occur less often than severe wind storms. On almost every day of the year, a severe wind storm is happening somewhere on Earth – although many storms are small and localized. In the tropical oceans, the most severe of all wind events – tropical cyclones (including hurricanes and typhoons) – are generated. When these storms make landfall on populated coastlines, their effects can be devastating. In this introductory chapter, the meteorology of severe wind storms – gales produced by large extra-tropical depressions – tropical cyclones and downbursts, squall lines, and tornadoes associated with thunderstorms, is explained, including the expected horizontal variation in wind speed during these events.
- 1. The nature of wind storms and wind-induced damage
- 2. Prediction of design wind speeds and structural safety
- 3. Strong wind characteristics and turbulence
- 4. Basic bluff-body aerodynamics
- 5. Resonant dynamic response and effective static load distributions
- 6. Internal pressures
- 7. Laboratory simulation of strong winds and wind loads
- 8. Low-rise buildings
- 9. Tall buildings
- 10. Large roofs and sports stadiums
- 11. Towers, chimneys and masts
- 12. Bridges
- 13. Transmission lines
- 14. Other structures
- 15. Wind loading codes and standards
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