Ocean currents are continuous, predictable, gravity-driven, wind (Coriolis Effect), and water abundance. Seawater travels in two directions: horizontally and vertically. Horizontal movements are referred to as waves, and vertical changes are called ups and downs. This abiotic system is responsible for heat transfer, biodiversity, and the Earth's climate system.


Types of Ocean Currents

Two types of ocean distribution: The ocean distribution derives its ocean energy from two sources that define two types of blood flow:


(1) Air-forced circulation, which puts pressure,


(2) A thermohaline-containing circulation of water and air, resulting in a radiant exchange. These two types of broadcasting are not entirely independent, since sea travel and hot air depend on wind speed. The wind-driven transmission has great potential in this and is set as the gyres that control the surface of the ocean. The air-driven stream is much stronger in the upper layer. The distribution of thermohaline is slow, with an average speed of 1 cm (0.4 inches) per second, but this flow enters the ocean and forms circular patterns covering the earth's oceans. sea ​​design


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