These currents are called LongShore or Feeder Currents.
Longshore currents
When waves move parallel to the shore, they are known as longshore currents. These currents can transport sediment along the coastline, resulting in the formation of features like sandbars and spits. Additionally, longshore currents can affect the erosion and deposition of coastal areas.
Long-shore currents are generated when waves approach the coast at an angle, causing water to move parallel to the shore. When waves hit the shore head on, there is less tendency for water to move laterally along the coast, resulting in weaker or non-existent long-shore currents.
Longshore currents are the movement of water within the surf zone that parallels the shore. These currents are responsible for transporting sand and sediment along the coastline and can be influenced by wave direction and beach topography. Longshore currents can be strong and pose a hazard to swimmers and surfers.
When waves tend to become parallel to the shore, it is called wave refraction. This occurs as waves change direction and bend towards the shore due to variations in water depth, causing them to align parallel to the shoreline.
Long shore currents form when waves approach the shoreline at an angle, causing the water and sediment to move parallel to the shore. This movement is a result of the wave's swash and backwash, creating a current that flows along the coastline. Long shore currents are influenced by wave direction, wave energy, and the shape of the coastline.
What are two kinds of near shore currents
A ridge of sand that runs parallel to the shore is called a sandbar. Sandbars are typically submerged or partially exposed at high tide and can be an important habitat for marine life.
Tidal outflows are called ebb currents. Ebb currents occur when water flows away from the shore as the tide goes out.
Riptides, also known as rip currents, are strong, narrow currents that flow from the shore back to the open ocean. They can pull swimmers out to sea and are dangerous for those caught in them. It is important to swim parallel to the shore if caught in a rip current to escape its pull.
Longshore currents transport sediment along the coastline parallel to the shore. These currents are driven by the waves hitting the coast at an angle, causing sediment to move in a zig-zag pattern along the shoreline.
Two kinds of currents that wave action can cause near shore are "Longshore Current", which is the overall direction and movement of the waves that strike the shore at an angle. The other kind of current is "Rip Currents", which are narrow streams of water that break through sandbars and drain rapidly back to sea.