the Coriolis effect.
Fast-moving rivers in the ocean are called ocean currents. These currents are driven by a combination of factors such as wind, water density, temperature, and the shape of the ocean floor. They play a crucial role in shaping global climate patterns and distributing heat around the Earth.
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.
Deep ocean currents are created by many elements. The first, is called the Thermohaline circulation, Thermo meaning hot and cold water interacting and haline meaning the amount of salt water verses fresh water, that changes places when ice melts and refreezes in the ocean. This circulation of cold rich salt water and warm surface water starts at the equator, where the water is warmed by the tropical sun and pushed ever north ward by cold dense water that flows from the poles. The second element that creates deep ocean currents is called the Coriolis effect, in physics this element is easiest explain by placing a rolling ball on a turning table. If the table where to remain stationary the ball when rolled would effectively roll straight and not deviate from its straight line. Where as with this effect if the ball where to be rolled while the table where in motion the ball would deviate from the straight line and roll off in the direction that the table is rolling in. As currents come from the poles they deviate from their straight path and fall along the continents. Thus creating deep ocean currents .
Circulating currents in a fluid are commonly referred to as convection currents. These currents arise due to the movement of the fluid caused by temperature differences, which lead to the transfer of heat within the fluid. Convection currents play a significant role in processes like ocean currents and the movement of air in the atmosphere.
Ocean currents can be measured using instruments such as current meters, Acoustic Doppler Current Profilers (ADCPs), and drifting buoys. These devices can provide information on the direction, speed, and depth of ocean currents. Remote sensing technologies, such as satellites, can also be used to measure surface currents over broader areas.
because of the Earths rotation the ocean currents are not in straight lines. In the northern hemisphere they curve to the right
because of the Earths rotation the ocean currents are not in straight lines. In the northern hemisphere they curve to the right
The rising of the deep cold currents to the ocean surface is called
Currents
IT'S called ocean currents or just called currents.
turbidty currents
Yes
They are called currents.
Fast moving rivers int he ocean are called currents. Currents are caused by the Earth's rotation. An ocean current is continuous.
Fast-moving rivers in the ocean are called ocean currents. These currents are driven by a combination of factors such as wind, water density, temperature, and the shape of the ocean floor. They play a crucial role in shaping global climate patterns and distributing heat around the Earth.
currents
Could it be Ocean-Atmosphere Coupling.