undertow
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.
Boiling water creates convection currents, where hot water rises and cooler water sinks. When you place an object in the boiling water, the convection currents cause the object to spin as the water moves around it.
The movement of water that runs next to the shore is called the littoral drift. This movement is influenced by waves, tides, and currents, and plays a crucial role in shaping the coastlines through erosion and sediment transport.
The downward force in water is due to gravity, which pulls objects towards the center of the Earth. This force is also known as buoyancy, and it is what allows objects to float or sink in water based on their density and displacement.
Surface tension is the force that pulls water up, slowing its downward movement. This force is due to the attraction between water molecules at the water-air interface. It causes water to form droplets and allows objects to float on its surface.
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.
waves and currents make the shore bigger
Objects in water or other fluids can be pushed up to the surface by buoyancy.
Flood currents occur when the tide is rising and water is moving towards the shore, while ebb currents occur when the tide is falling and water is moving away from the shore. Flood currents typically bring in nutrient-rich water and are associated with higher water levels, while ebb currents can be stronger and are associated with lower water levels. Both currents can influence navigation, sediment transport, and marine life in coastal areas.
Currents within the surf zone that flow parallel to the shore are known as longshore currents. These currents are generated by waves approaching the shore at an angle, creating a flow of water along the coastline. Longshore currents can significantly influence sediment transport and beach erosion, shaping coastal landscapes over time. They often interact with rip currents, which flow seaward and can pose hazards to swimmers.
Tidal outflows are called ebb currents. Ebb currents occur when water flows away from the shore as the tide goes out.
When water reaches the shore, it can form various landforms such as beaches, sandbars, spits, and lagoons. Waves and currents play a role in shaping these coastal features.
Surface ocean currents are caused by winds. As wind blows across the surface, the wind pulls the water and causes waves.
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.
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.
Longshore currents are driven by the angle at which waves approach the shore. When waves hit the shore head-on, rather than at an angle, there is no net transport of water along the shoreline to generate a longshore current. The wave energy is dissipated directly onto the shore, preventing the development of a longshore current.
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.