deep water waves

Deep water waves are surface waves that occur in water deeper than half their wavelength. Their movement involves both water particles moving in circular or elliptical paths as the wave passes, with the particle motion decreasing with depth. These waves are primarily generated by wind and travel across open oceans. Because they exist in deep water, their properties—such as speed and height—depend mainly on the wave’s wavelength and the water’s gravity, rather than the ocean bottom. They are distinct from shallow water waves, which are influenced by the seabed and can slow down or grow taller as they approach shore.