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What is the driving force of deep-ocean circulation?

The driving force of deep-ocean circulation is primarily the sinking of cold, dense water at high latitudes due to its higher density. This process is known as thermohaline circulation, where temperature and salinity differences create variations in water density, causing water masses to sink and drive the global ocean circulation.


Which sequence of processes transports water from the atmosphere to the ocean and then back into a cloud?

Evaporation and condensation transport water from the ocean into a cloud.


How does atmospheric forcing impact the dynamics of ocean circulation?

Atmospheric forcing, such as wind and temperature changes, can affect ocean circulation by influencing the movement of surface waters and the formation of ocean currents. These forces can drive the mixing of water masses, impact the distribution of heat and nutrients, and play a role in shaping the overall circulation patterns of the ocean.


What is deep water formation?

Deep water formation is the process by which surface waters in the ocean cool and become denser, sinking to the depths of the ocean. This sinking of dense water drives the global thermohaline circulation, which plays a key role in distributing heat and nutrients around the world's oceans. Deep water formation is crucial for ocean circulation and climate regulation.


How do the shape of the ocean basins and density differences in ocean water influence its movement?

The shape of ocean basins influences the direction and flow of ocean currents through the Coriolis effect. Density differences in ocean water, caused by temperature and salinity variations, drive vertical mixing and circulation patterns, such as thermohaline circulation, which play a crucial role in redistributing heat and nutrients around the globe.

Related Questions

Name for the worldwide circulation of the ocean currents which transport warm water to colder areas and cold water to warmer areas?

Global Conveyor Belt


What is the driving force of deep-ocean circulation?

The driving force of deep-ocean circulation is primarily the sinking of cold, dense water at high latitudes due to its higher density. This process is known as thermohaline circulation, where temperature and salinity differences create variations in water density, causing water masses to sink and drive the global ocean circulation.


Circulation of ocean water is called?

Current


What is the circulation of water mostly responsible for?

Deep water ocean current


What is efficiently transported due to the circulation of the ocean water?

Heat.


What is the Atlantic thermohaline circulation?

The Atlantic thermohaline circulation, also known as the Atlantic Meridional Overturning Circulation (AMOC), is a large system of ocean currents that transport warm, salty water northward in the Atlantic Ocean and colder, fresher water southward. It plays a crucial role in regulating Earth's climate by distributing heat around the globe. Disruption of the AMOC can have significant impacts on regional and global climate patterns.


Which sequence of processes transports water from the atmosphere to the ocean and then back into a cloud?

Evaporation and condensation transport water from the ocean into a cloud.


What is a possible cause that the Atlantic Ocean water is slightly less dense than the average water of any other ocean?

Thermohaline circulation is the process of cold water at the poles creeping along the ocean floor. It meets with north and south polar water creates a dawdling subsurface circulation.


What drives deep ocean currents are driven?

Deep ocean circulation(90% of ocean water) is caused by differences in temperature, salinity and suspended load. It is referred to as "Thermohaline"- meaning heat and salt- circulation.


What do you call the circulation in ocean that brings deep cold water to the surface?

Ocean convection currents move the deep cold water to the surface of oceans.


What is the driving force of oceanic?

Deep ocean circulation(90% of ocean water) is caused by differences in temperature, salinity and suspended load. It is referred to as "Thermohaline"- meaning heat and salt- circulation.


How does atmospheric forcing impact the dynamics of ocean circulation?

Atmospheric forcing, such as wind and temperature changes, can affect ocean circulation by influencing the movement of surface waters and the formation of ocean currents. These forces can drive the mixing of water masses, impact the distribution of heat and nutrients, and play a role in shaping the overall circulation patterns of the ocean.