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Hurricane winds are unique in several ways: <br /> • They are more turbulent than winds in most other types <br /> of storms; <br /> • They are sustained for a longer period of time (several <br /> hours)than any other type of atmospheric disturbance; <br /> • They change slowly in direction; thus, they are able to <br /> seek out the most critical angle of attack on a given <br /> structure; and <br /> • They generate large quantities of flying debris as the <br /> built environment is progressively damaged; thus, <br /> amplifying their destructive power. <br /> In hurricanes, gusts of wind can be expected to exceed the <br /> sustained wind velocity by 25% to 50%. This means a <br /> hurricane with sustained winds of 150 mph will have wind <br /> gusts exceeding 200 mph. The wind's pressure against a fixed <br /> structure increases with the square of the velocity. For <br /> example a 100-mph wind will exert a pressure of approximately <br /> 40 pounds per square foot on a flat surface, while a 190-mph <br /> wind will exert a force of 122 pounds per square foot on that <br /> same structure. In terms of a 4- by 8-foot sheet of plywood <br /> nailed over a window, there would be 1,280 pounds of <br /> pressure against this sheet in a 100-mph wind, and 3,904 <br /> pounds or 1.95 tons of pressure against this sheet in a 190- <br /> mph wind. <br /> The external and internal pressures generated against a <br /> structure vary greatly with increases in elevation, shapes of <br /> buildings, openings in the structures, and the surrounding <br /> buildings and terrain. Buildings at ground level experience <br /> some reductions in wind forces simply because of the drag <br /> exerted by the ground against the lowest levels of the air <br /> column. High-rise buildings, particularly those located along <br /> the beachfront will receive the full strength of hurricane winds <br /> on their upper stories. Recent studies estimate that wind <br /> speed increases by approximately 37% just 15 feet above <br /> ground level. <br /> The wind stream generates uplift as it divides and flows around <br /> a structure. The stream following the longest path around a <br /> building, generally the path over the roof, speeds up to rejoin <br /> the wind streams following shorter paths, generally around the <br /> walls. This is the same phenomenon that generates uplift on <br /> Indian River County Comprehensive Emergency Management Plan Basic Page 14 <br />