Sunlight warms the waters on the ocean surface. Some heat energy is transferred to cooler waters through convection.
Quatic is when the ocean's currents get gigantic and creates a tsunami.
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Wind can impact ocean currents by transferring energy to the surface of the water, causing it to move in the direction of the wind. This creates surface currents that can influence the direction and speed of deeper ocean currents. Strong winds over a large area can lead to the formation of powerful currents, such as the Gulf Stream.
The mantle's convection currents move in the mantle in the form of magma which creates the mid-ocean ridge. Mid-ocean ridges are found in every ocean in the world and when the currents erupt as lava the eventually cool and create a crust.
Sunlight warms the waters on the ocean surface. Some heat energy is transferred to cooler waters through convection.
The term that describes the upper part of the ocean into which sunlight penetrates is called the "euphotic zone." This is where photosynthesis occurs as sunlight is able to reach the surface layers of the ocean, supporting the growth of phytoplankton and other marine plants.
Ocean currents are primarily caused by wind patterns, the Earth's rotation (Coriolis effect), and differences in water density due to temperature and salinity variations. Surface currents are driven by winds, while deep ocean currents are influenced by density differences and temperature gradients. The combination of these factors creates the two types of ocean currents.
An ocean current is a continuous, directed movement of ocean water generated by the forces acting upon this mean flow, such as breaking waves, wind, Coriolis effect,cabbeling, temperature and salinity differences and tides caused by the gravitational pull of the Moon and the SunFrom Wiki
Cold ocean currents sink under warm ocean currents to form deep ocean currents.
The rotation of Earth causes the apparent path of ocean currents to curve
Ocean currents is what forms surface currents. This starts deep in the ocean.