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Yucatán Channel

geography Maturity 5-7 Next article →

The Yucatán Channel is a busy path of water. It sits between Mexico and Cuba. This strait links the Caribbean Sea to the Gulf of Mexico. It runs from Cape Catoche in Mexico to Cape San Antonio in Cuba. It helps move water between these two large bodies of water. This channel is a very important part of the ocean.

Water moves through this channel in many different ways. Most of the water flows from east to west. This flow is made of two main parts. One part comes from the North Equatorial Current. The other part comes from the South Equatorial Current near Brazil. Together, they create a huge flow of 17 Sv. This water stays at a temperature of at least 25 degrees Celsius.

As this water moves past the Yucatán Peninsula, it changes. It becomes known as the Yucatán Current. This current brings most of the water into the Gulf of Mexico. It flows very strongly on the western side of the channel. On the eastern side, the Cuban Countercurrent flows the opposite way. There is also a deep Yucatán Undercurrent that flows south. This undercurrent takes water away from the Gulf.

Near the coast of Cuba, the water reaches its deepest point. As the water moves into the Gulf, it hits the Campeche Bank. This is a shallow area of the sea. Coral reefs grow on the outer edges of the Yucatán shelf. Three main types of coral live here. These are Acropora cervicornis, Acropora palmata, and Montastraea annularis. Many of these corals died in the late 1990s. Some have since started to grow back.

This area is full of many different living things. The Campeche Bank is a very biodiverse place. Because of this, many people come here to fish. Artisan fishermen travel from the Mexican coast to these waters. They work hard to catch fish in this area. However, the area faces a threat from overexploitation. This means people might take too many living things from the sea.

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