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Concept:wind*Development of Wind Wind usually refers to the movement of air parallel to the earth's surface. The driving forces of winds in the lowest few hundred feet of the atmosphere are pressure differences caused by unequal heating of the air. The direction is also affected by the Coriolis force. Normally, wind requires several hours to develop.
*Velocity Profile The roughness of the earth's surface causes the surface wind speed to be much less than the wind speed at higher levels. Velocity profiles have been determined by fitting curves to observed mind speeds at several levels, is described by a power law of the form: Vh = Vr*(h/hr)^k where Vh is the mean wind speed at height h above the ground, Vr is the mean speed at the reference height h (10 metres or about 30 feet is internationally recommended as the standard), above the ground, k is the exponent for the best-fitting curve.
*Turbulence in Surface Winds Superimposed on the mean speed are gusts and lulls. These gusts have a random distribution over a wide range of frequencies and amplitudes, both in time and space.
*Design Wind Speeds The basic design wind load in the National Building Code of Canada is the velocity pressure of a wind lasting for a few seconds that will be exceeded on the average once in 30 years.
Wind loads have become particularly significant because of the increasing number of high-rise buildings. Other factors have also contributed to the importance of wind in design: light-weight low-slope roofs, curtain wall construction and the appearance of special structures having "aerodynamic shapes."
Wind loads have become particularly significant because of the increasing number of high-rise buildings. Other factors have also contributed to the importance of wind in design: light-weight low-slope roofs, curtain wall construction and the appearance of special structures having "aerodynamic shapes."
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