Much of the destruction caused by a hurricane comes from the sea. The low pressure in the eye sucks up the sea beneath, raising it by as much as 6m (20ft). At the same time, violent winds whip up waves as tall as houses. The high water level and the freak waves combine to make “storm surges” — towering walls of seawater that surge inland for many kilometres, sweeping away buildings, trees and anything in their path.
A storm surge is a rise in sea level that occurs during tropical cyclones, intense storms also known as typhoons or hurricanes. The storms produce strong winds that push the water into shore, which can lead to flooding. This makes storm surges very dangerous for coastal regions.
Tropical cyclones are circular storms characterized by high winds and heavy rainfall. They form over warm, tropical oceans. The center of a cyclone is called the eye. The eye is surrounded by a ring of clouds called the eye wall, where the winds are strongest. Surrounding the eye wall are clouds that spiral outward, called spiraling rain bands.
A storm surge is primarily caused by the relationship between the winds and the ocean’s surface. The water level rises where the winds are strongest. In addition, water is pushed in the direction the winds are blowing. The rotation of the Earth causes winds to move toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere—a phenomenon known as the Coriolis effect. If a cyclone develops in the Northern Hemisphere, the surge will be largest in the right-forward part of the storm. In the Southern Hemisphere, the surge will be largest in the left-forward part of the cyclone.
Another factor contributing to storm surge is atmospheric pressure. Atmospheric pressure is the force exerted by the weight of air in the Earth’s atmosphere. The pressure is higher at the edges of a cyclone than it is at the center. This pushes down the water in the outer parts of the storm, causing the water to bulge at the eye and eye wall—where the winds have helped add to the rise in sea level.
More factors contribute to the strength of a storm surge as the dome of water comes ashore. The water level can reach as high as 10 meters (33 feet) if the storm surge happens at the same time as high tide. The slope of the land just off the coast also plays a part: Water will more easily flood a shallow coast than a steep one.
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