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Winds and ocean currents move water parallel to Earth's surface. Winds can create surface currents through friction with the ocean's surface, while ocean currents are driven by a combination of factors such as wind, temperature, salinity, and the Earth's rotation.
Surface waves are where particles of the medium move both parallel and perpendicular to wave motion. This movement creates a circular motion pattern. An example of a surface wave is water waves on the surface of a pond.
Longshore currents shift sand and move water parallel to the shoreline
deepwater currents
Transverse waves oscillate perpendicular to the direction of energy propagation. Think of one wave by itself. Which direction is it propagating? Some direction parallel to the surface of the water. Now think of one particular piece of water that the wave passes through. It's motion goes upwards and downwards, which is perpendicular from the surface of the water, therefore transverse. Waves oscillating parallel to the direction of energy propagation are called longitudinal.
Currents powered by wind are called wind-driven currents or wind-driven circulation. These currents are created by the friction between the wind and the surface of the water, causing the water to move in the direction of the wind.
The energy that drives the movement of the water
Surface ocean currents are caused by winds. As wind blows across the surface, the wind pulls the water and causes waves.
surface currents are horizontal, steamlike movements of water that are found at or near the surface of the ocean
The three types of ocean currents are surface currents, deep currents, and tidal currents. Surface currents are driven by winds, deep currents are driven by density and temperature differences, and tidal currents are driven by the gravitational pull of the moon and sun.
Surface Currents.
With water or oceanic currents, the currents which move close to the surface of the sea are called surface currents. In such currents, wind acts on the water and the water piles up to form strong movement forces.