Tides at charleston Charleston, located on a coastal plain, experiences mixed semidiurnal tides, which means there are two high tides and two low tides each day, with slightly unequal heights. This tide pattern is common along the U.S. East Coast and is mainly influenced by the moon's gravitational pull. The sun also plays a role, causing higher high tides and lower low tides during full and new moons (spring tides) and smaller differences during first and third quarter moons (neap tides). The tidal range, or the difference in height between high and low tide, varies throughout the month and year. In Charleston, the average tidal range is about 5.5 feet (1.67 meters), but it can reach up to 7 feet (2.13 meters) during spring tides. The timing of tides also shifts daily due to the Earth's rotation, making it essential to consult up-to-date tide predictions. Tides in Charleston are further influenced by the shallow continental shelf and the nearby Frying Pan Shoals, a large sandbar that extends about 20 miles (32 kilometers) southeast of Cape Fear, North Carolina. These geographical features can amplify tidal ranges and cause local variations in tidal currents. Tidal currents, the horizontal movement of water associated with the rise and fall of tides, are essential for boat navigation and aquatic ecosystems. In Charleston, tidal currents can reach speeds of 2 to 3 knots (3.7 to 5.6 km/h) in some areas, particularly around inlets, channels, and other constricted areas. Cooper City Commons is a popular shopping center located in the heart of Cooper City, Florida. The plaza is home to a wide variety of stores, restaurants, and services, making it a one-stop-shop for residents and visitors alike. Charleston, located on a peninsula between the Ashley and Cooper rivers, experiences a mixed tide system, characterized by two high tides and two low tides every lunar day (24 hours and 50 minutes). This is because Charleston is situated on the Atlantic coast, where the semidiurnal tide (two high and two low tides per day) is the primary tidal pattern. The range of tides, which is the difference in height between high tide and low tide, varies throughout the month and year. The mean tidal range in Charleston is about 5.5 feet, but it can reach up to 7 feet during spring tides and decrease to around 3.5 feet during neap tides. Spring tides occur when the sun, Earth, and moon are aligned, amplifying the gravitational forces and leading to higher high tides and lower low tides. Neap tides occur when the sun and moon are at right angles to each other relative to the Earth, reducing the gravitational forces and leading to smaller tidal ranges. The tidal currents in Charleston are also an essential aspect of the tide system. These currents are responsible for the movement of water in and out of the harbor and are affected by the shape of the coastline, water depth, and wind. The ebb current, which flows out of the harbor, typically occurs during low tide, while the flood current, which flows into the harbor, takes place during high tide. Tides in Charleston are influenced by the shape of the continental shelf, which gradually slopes offshore, and the presence of the Charleston Bump, an underwater feature located about 150 miles southeast of the city. The Charleston Bump affects tides by altering the path of tidal currents and creating complex tidal patterns.
7. **Fogo de Chão** (117 E. Washington St.): If you're in the mood for a Brazilian steakhouse experience, Fogo de Chão is the place to go. This upscale restaurant features a variety of grilled meats, along with a salad bar and other sides.