WAVES, OCEAN CURRENTS AND TIDES
Ocean waves are rhythmic disturbances that transfer energy across the surface of the water, primarily generated by the wind. They play a fundamental role in shaping coastlines, driving ocean currents, and affecting marine ecosystems. Waves can travel vast distances across oceans, transferring energy rather than water. Waves vary greatly in size, strength, and duration, depending on their formation process and environmental conditions.
Waves are primarily formed by the action of wind on the surface of the water. When wind blows over the ocean, friction between the air and water causes ripples. As these ripples grow, they become larger waves through a process known as wave growth by wind action. The three main factors that influence the size and power of the waves are:
1.Wind Speed: The stronger the wind, the more energy is transferred to the water, resulting in larger waves.
2.Duration: The longer the wind blows over the water, the more time the waves have to grow in size.
3.Fetch: Fetch refers to the distance over which the wind blows across the water without interruption. A longer fetch allows waves to gather more energy, resulting in larger and more powerful waves. For example, the Southern Ocean around Antarctica has some of the largest waves in the world because it has a very long fetch with minimal land barriers.
In addition to wind, other forces such as earthquakes, volcanic eruptions, and gravitational forces from the moon and sun can also generate waves, particularly tsunamis and tidal waves.