The combined effects of sediment transport within the surf zone by the longshore current and sediment movement along the beach by swash and backwash is known as longshore transport , or littoral drift .
As the ocean's surface waves reach the coast, they get bigger and shatter, creating the foamy, bubbly surface known as surf. The surf zone, also known as the breaker zone, is defined by the region of breaking waves.
The surf zone is that relatively short strip of a body of water that borders the shore and features breaking waves due to the shallow water depth.
The surf zone, also known as the breaker zone, is defined by the region of breaking waves. After breaking in the surf zone, the waves continue to advance in and flow up onto the sloping front of the beach, generating an uprush of water known as swash. The water then returns as backwash.
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