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Large-scale ocean water circulation driven by density is known as thermohaline circulation. This process is primarily influenced by variations in water temperature (thermal) and salinity (haline), which affect water density. Cold, salty water is denser and sinks in polar regions, while warmer, less salty water rises in equatorial regions, creating a global conveyor belt of ocean currents. This circulation plays a crucial role in regulating climate, distributing heat, and influencing marine ecosystems worldwide.
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Surface ocean circulation is also called thermohaline circulation?
Thermohaline circulation is also called overturning circulation. It is driven by density. The time scale for thermohaine is 1000 years.
When the sun heats one region in an ocean the movement of the water in the ocean circulates the leat What is the name of this phenomenon?
The phenomenon you are describing is known as ocean circulation or thermohaline circulation. This process is driven by differences in temperature and salinity in the water, which create density variations that cause the water to move. The circulation helps distribute heat across the ocean, influencing climate and weather patterns. A specific component of this is the "ocean conveyor belt," which refers to the large-scale movement of water that connects different ocean basins.
Thermohaline circulation is driven by changes in?
Thermohaline circulation is driven by changes in temperature and salinity of ocean water. Cold, dense water sinks in the polar regions due to its high salinity and low temperature, driving the deep ocean currents that help regulate the global climate by redistributing heat and nutrients around the world.
What factors include the direction of ocean currents?
The factors that can modify the currents are direction and shape of coastlines, bottom reliefs of the ocean basins, seasonal variations and rotation of the earth. Ocean circulation is driven by winds and by differences in water density
Do density currents ocour in the pacific ocean?
Yes, density currents occur in the Pacific Ocean, as they do in other oceanic regions. These currents are driven by differences in water density, which can result from variations in temperature and salinity. In the Pacific, processes such as upwelling and downwelling contribute to the formation of density currents, impacting nutrient distribution and marine ecosystems. Such currents play a crucial role in the ocean's thermohaline circulation.
Another name for the thermohaline current is?
The thermohaline circulation is a term for the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water
What is Thermohaline circulation is driven by differences in?
Thermohaline circulation is driven by differences in temperature and salinity in the ocean, which affect water density. Warm, less saline water is less dense and tends to rise, while cold, saline water is denser and sinks. This creates a global conveyor belt of ocean currents that plays a crucial role in regulating climate, distributing heat, and supporting marine ecosystems. The interplay of these factors helps drive the large-scale movement of water across the world's oceans.
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 is a large wind driven surface currents that create circular movements in the ocean?
What is a large wind driven surface currents that create circular movements in the ocean?
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.
What do you call deep ocean circulation driven largely by variations in water temperature and salinity?
thermohaline
What forces dive deep ocean currents?
Deep ocean currents are primarily driven by two main forces: thermohaline circulation and wind. Thermohaline circulation is influenced by variations in water density, which is affected by temperature (thermo) and salinity (haline). As surface water cools and becomes saltier, it sinks, creating a global conveyor belt of deep ocean currents. Additionally, wind-driven surface currents can also influence deeper currents through the process of upwelling and downwelling.
