Question 5.9: The Rise of the Ocean Due to a Hurricane A hurricane is a tr...
The Rise of the Ocean Due to a Hurricane A hurricane
is a tropical storm formed over the ocean by low atmospheric pressures. As a hurricane approaches land, inordinate ocean swells (very high tides) accompany the hurricane. A Class-5 hurricane features winds in excess of 250 km/h, although the wind velocity at the center “eye” is very low.
Figure 5–43 depicts a hurricane hovering over the ocean swell below. The atmospheric pressure 320 km from the eye is 762 mm Hg (at point 1, generally normal for the ocean) and the winds are calm. The atmospheric pressure at the eye of the storm is 560 mm Hg. Estimate the ocean swell at (a) the eye of the hurricane at point 3 and (b) point 2, where the wind velocity is 250 km/h. Take the density of seawater and mercury to be 1025 kg/m³ and 13,600 kg/m³, respectively, and the density of air at normal sea-level temperature and pressure to be 1.2 kg/m³.
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