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Waves change direction as they approach shore due to the shallowing of water depth. This causes the wave to slow down and bend towards shallower areas. This process is known as wave refraction.
nearly parallel to the shoreline
Waves change direction near shore due to shoaling, which is the process of waves slowing down and increasing in height as they move into shallower water. This change in speed and height causes the waves to bend, aligning more parallel with the shoreline. The energy in the waves is also compressed which results in them breaking as they reach the shore.
Waves change direction as they near shore due to the interaction between the wave front and the sea bottom. This interaction causes the wave to slow down and bend, resulting in the wave refraction. Refraction causes the wave energy to focus on headlands and disperse in bays, affecting wave direction.
As waves approach the shore, their wavelength decreases, causing the waves to grow in height. This phenomenon is known as wave shoaling. Additionally, wave velocity decreases as they enter shallower water near the shore.
As waves approach the shore, their height increases, and their speed decreases due to the interaction with the sea floor. The wave crests become steeper and eventually break as the waves approach the shallow water near the shore.
As waves approach a shore, they typically increase in height and decrease in length. This is due to the interaction with the shallow water near the shore, causing the wave to slow down and compress. The wave may also break as it gets closer to the shore, leading to the formation of surf.
The direction of a longshore current can reverse due to changes in wave direction, which may occur with shifts in wind patterns or tidal movements. When waves approach the shore at different angles, they can alter the flow of water along the coastline. Additionally, coastal features like jetties or groins can disrupt the current, causing it to change direction. Seasonal variations in wave energy and storm activity can also contribute to these reversals.
nearly parallel to the shoreline
As waves approach the shore, they experience shoaling which causes them to slow down and increase in height. This is due to the decrease in water depth and the wave energy becoming compressed. The waves then break as they reach shallower waters, eventually dissipating their energy on the shore.
As waves approach the shore, their height increases, causing them to become steeper and eventually break. The wavelength decreases as the wave interacts with the shallower water near the shore. This process is known as wave shoaling.
The long shore current will typically flow parallel to the beach in a northeast or southeast direction following the direction of the incoming waves from the southwest. This current is generated as the waves push water along the shoreline, causing a movement of water in the same direction as the wave approach.