I don't know what you're asking as this is not phrased as a question.
The swash zone is the part of a beach shore where the waves crash.
if you mean backwash (the opposite to swash) its the water of a wave travelling back down a beach, transporting beach material, due to gravitational forces :)
Waves going back and fourth.
In summer, swash and backwash at a beach will typically be more energetic and stronger due to increased wave activity caused by stronger winds and storms. This can result in higher waves and a more forceful movement of water up the beach during swash and back down during backwash. In contrast, during winter, swash and backwash may be less pronounced as wave energy decreases, resulting in smaller waves and less forceful water movement on the beach.
Swash and backwash waves are associated with coastal deposition. Swash waves carry sediment onto the beach, while backwash waves transport sediment back into the ocean. This back-and-forth movement helps build up beaches and contribute to coastal deposition processes.
If the swash is bigger than the backwash, it results in the accumulation of sediment on the beach, leading to a build-up of sand. This occurs because the stronger swash pushes more material up the shore, while the weaker backwash struggles to pull it back down. Over time, this can create wider and more pronounced beach profiles. Additionally, the excess sediment can affect coastal ecosystems and habitats.
A constructive interference wave, where two waves combine to create a larger wave, can produce a swash stronger than the backwash. This can happen when the incoming waves are longer in wavelength and have a higher wave height, causing the swash to carry more water up the beach than the backwash can pull back down.
gravity pulling it back towards the ocean as the wave recedes.
The water that moves up the beach in a wave flows back out to sea due to gravity pulling it back towards the ocean. This process is known as backwash and it helps to reset the balance of water levels between the beach and the ocean.
The primary force responsible for moving sand along a beach is wave action, particularly the swash and backwash generated by breaking waves. As waves approach the shore, they carry sand up the beach (swash), and then gravity pulls it back down (backwash). Additionally, prevailing wind patterns can also contribute to the movement of sand, especially in shaping dunes and beach profiles. Together, these processes create a dynamic system that redistributes sand along the coastline.
The swash process occurs at an angle primarily due to the prevailing direction of waves approaching the shore, which are influenced by wind and ocean currents. As waves break on the beach, the water moves up the slope of the shore at an angle, driven by the wave's energy. Gravity then pulls the water back down the slope, creating a backwash that typically flows straight down. This angled movement results in a net sediment transport along the shore, contributing to coastal erosion and deposition patterns.
Wave behavior that can bring a gold coin close to shore includes breaking waves and swash. When waves approach the shore, they break and lose energy, causing sediment and objects like a gold coin to be pushed forward by the swash—the water that moves up the beach after a wave breaks. Additionally, backwash can pull some materials back, but the overall effect of breaking waves typically results in objects being deposited closer to the shore.
Material can be transported along a beach via longshore drift;Waves approach beach at an angleMaterial is pushed up the beach by the swash in the same direction as the wave approachAs the water runs back down the beach the backwash drags material down at right angles to the beach lineOver a period of time sediment moves in this zig-zag fashion down the coast.Material can also be transported along a beach at low tide when the sand dries out by the wind (usually forming sand dunes)Material may also be transported up and down a beach by attrition. Waves may have fairly high energy so will pick up material and may loose energy further up the beach and therefore deposit it there.Might also be moved by saltation (waves carry slightly smaller sediment in the same way as attrition)Waves may be swash-aligned (waves hit beach straigt on, so sediment moved up and down beach) or drift-aligned (waves hit beach at right angles causing longshore drift)