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The Gulf of Mexico is a low-energy, microtidal (less than 0.5 m tidal amplitude) region that is constantly changing as a result of active coastal processes that are directly linked to meteorological events. Wind-driven waves and tidal currents are the most important geological agents controlling sediment transport and evolution of the Gulf and bay shores. Depending on location, the morphological features can be wave-dominated, tide dominated, or display mixed energy characteristics of both wave and tidal influences (Davis, 1994). Wind directions and intensities vary seasonally with southeasterly and southwesterly winds prevailing most of the year. Exceptions occur frequently during the winter months when wind-circulation patterns and low barometric pressure preceding the passage of cold fronts cause strong onshore winds and high waves that erode the beach. After the frontal systems pass the coast, winds shift to blow from the northwest or northeast, causing erosion along the lagoon sides of the barriers and the southwestward transport of sediment in the Gulf of Mexico.
Astronomical tides in the Gulf of Mexico are mixed and typically have a range of less than 1 m. Water levels vary only about 0.5 m between high and low tide during a normal tidal cycle. Tide records around the Gulf since the turn of the century all show the same general variations in sea level that coincide with droughts and periods of abnormally high rainfall. Averaging of the tide records shows that some areas such as the west-central coast of Florida are relatively stable because of the hard limestone substrates. Other areas, such as the Mississippi delta and around Galveston, Texas are subsiding rapidly.
Non-storm waves in the Gulf of Mexico are about 0.3 m high. The largest waves and highest sustained wind speeds in the Gulf accompany major hurricanes, which also are responsible for the most storm-related property damage and loss of lives. Hurricanes entering or originating in the Gulf normally follow a northward or westward path. Using historical patterns of hurricane landfall, the National Hurricane Center has shown that the areas at greatest risk are around Galveston, Texas, southeastern Louisiana, and the Mississippi/Alabama coast (Simpson and Lawrence, 1971). Because hurricanes seldom turn east and make landfall near the west Florida coast, this area has the lowest probability of a storm in any year.
Before crossing the Gulf Coast, the counterclockwise circulation of hurricane winds drives nearshore currents and large volumes of beach sand alongshore. The high tides, large waves, and strong currents that accompany the storms can leave a permanent mark on the barrier islands and beaches. For example, the 1921 Hurricane breached Hog Island and formed Hurricane Pass that now separates Honeymoon Island from Caladesi Island. Even relatively weak storms have destroyed piers, seawalls, dune walkovers, swimming pools, roads, houses, motels, and other buildings because structures were located close to the water and the beach did not recover from storm erosion before the next storm arrived.
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