In open sea, despite the vertical motion of the sea, there is little horizontal transfer. Ot is only when waves approach the shore that there is a forward movement of water as waves break and wash up the beach.
The seabed interrupts the circular orbital movement of the water. As the water becomes shallower the circular motion becomes more eliptical. This causes the crest of the wave to rise up and then eventually topple onto the beach.
The water that rushes up the beach is called the swash. The water that flows back towards the sea is called the backwash.
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