Factors that set surface ocean currents into motions are the global circulation cells (Hadley, Ferrel, Polar), the Coriolis effect, and the continental deflection.
Continental deflections,the Coriolis effect and global winds all effect surface ocean currents.
the sun and erosion
Ocean currents is what forms surface currents. This starts deep in the ocean.
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.
Currents, tides, & waves.
Deep ocean currents and surface currents do interact and influence each other. While they flow at different depths and have different driving factors (wind for surface currents and density for deep currents), they are connected through the global ocean circulation system. Changes in one can impact the other over time.
Surface ocean currents are caused by winds. As wind blows across the surface, the wind pulls the water and causes waves.
Deep ocean currents are in the depths of the oceans. Surface current are at the surface, not deep down. Deep ocean currents bring vitamins and nutrients to the shore, surface currents do not. Deep ocean currents are caused by salinity and temperature differences. Surface currents are cause by the force and impact of the wind.
Deep ocean currents are in the depths of the oceans. Surface current are at the surface, not deep down. Deep ocean currents bring vitamins and nutrients to the shore, surface currents do not. Deep ocean currents are caused by salinity and temperature differences. Surface currents are cause by the force and impact of the wind.
Continental deflections,the Coriolis effect and global winds all effect surface ocean currents.
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.
In the Northern Hemisphere, ocean surface currents generally flow clockwise due to the Coriolis effect. This means currents tend to move to the right in the northern hemisphere. However, local factors such as winds, coastal topography, and temperature gradients can also influence the direction of ocean currents.