deep ocean currents form by the differences in the density of ocean water
Deep currents form by the differences in the density of the ocean water. Deep currents move by carrying cold water from the poles towards the equators. They flow really slowly. They may take as long as 1,000 years to flow from the pole to the equator and back again.
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.
The ocean currents known since antiquity are called surface currents. Though these are invaluable to shipping, they are superficial and occupy only a small fraction of the ocean's waters. The majority of the ocean's currents take the form of a temperature- and salinity-driven "conveyor belt" that slowly churns water within the abyssal depths. These loops of water circulation are called deep currents.
The two main ocean circulation patterns are surface currents and deep ocean currents. Surface currents are driven by the wind and are influenced by the Earth's rotation, leading to the formation of gyres. Deep ocean currents are driven by differences in water density caused by temperature and salinity variations. These currents play a crucial role in distributing heat and nutrients around the globe.
The heating of the ocean surface by the sun is the PRIMARY source of energy that drives the ocean currents. How and where they move is dependent on the spinning of the earth, wind patterns and the positions of the continents and oceans and the cool polar areas. In effect the ocean current transfer (solar) heat form the tropics to the poles and even out the temperature variations across the planet. winds, gravity, and water density are factors that move ocean currents.
Ocean convection currents move the deep cold water to the surface of oceans.
Deep currents form by the differences in the density of the ocean water. Deep currents move by carrying cold water from the poles towards the equators. They flow really slowly. They may take as long as 1,000 years to flow from the pole to the equator and back again.
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.
Ocean currents form
The ocean currents known since antiquity are called surface currents. Though these are invaluable to shipping, they are superficial and occupy only a small fraction of the ocean's waters. The majority of the ocean's currents take the form of a temperature- and salinity-driven "conveyor belt" that slowly churns water within the abyssal depths. These loops of water circulation are called deep currents.
These currents make up 90% of the ocean waters.These waters move around the ocean basins due to variations in the density and gravity.Deep waters sinks into the deep ocean basins at high latitudes , where the temperatures are cold enough to cause the density to increase.
Ocean currents.
Deep water currents are primarily driven by differences in water temperature and salinity, which affect water density. When denser, colder, or saltier water sinks, it can create deep currents that move along the ocean floor. Other factors such as wind patterns, Earth's rotation, and underwater topography can also influence deep water currents.
The two main ocean circulation patterns are surface currents and deep ocean currents. Surface currents are driven by the wind and are influenced by the Earth's rotation, leading to the formation of gyres. Deep ocean currents are driven by differences in water density caused by temperature and salinity variations. These currents play a crucial role in distributing heat and nutrients around the globe.
The heating of the ocean surface by the sun is the PRIMARY source of energy that drives the ocean currents. How and where they move is dependent on the spinning of the earth, wind patterns and the positions of the continents and oceans and the cool polar areas. In effect the ocean current transfer (solar) heat form the tropics to the poles and even out the temperature variations across the planet. winds, gravity, and water density are factors that move ocean currents.
its easy for them to move
Yes