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.
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.
Ocean currents at the SURFACE -- their primary cause is SOLAR ENERGY. Due to solar energy, much of the wind pattern originates and this wind pattern in turn causes ocean currents on the surface.
Ocean currents is what forms surface currents. This starts deep in the ocean.
Compare and contrast surface currents and deep currents. They are both are moving water that flows through oceans. Surface currents are towards the top of the ocean, can be warm or cold, and are controlled by winds. Deep currents are low, deep in the ocean, cold, and are controlled by density.
The circulation of cold and warm water between the poles and the equator, and the rotation of the earth, cause ocean currents to flow.
Surface
Surface ocean currents are caused by winds. As wind blows across the surface, the wind pulls the water and causes waves.
Global winds do not directly cause deep currents. Deep ocean currents are primarily driven by differences in water density, which are influenced by temperature and salinity. While global winds can indirectly affect the distribution and movement of deep currents through their impact on surface currents and mixing processes, they are not the primary driving force.
Surface currents are primarily caused by the wind, which transfers its energy to the ocean's surface through friction. The rotation of the Earth also influences the direction of these currents through the Coriolis effect.
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.
The rising of the deep cold currents to the ocean surface is called