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Dense water can remain on the ocean floor for extended periods, often ranging from decades to centuries. This is particularly true for deep ocean currents, which are part of the thermohaline circulation. The longevity of dense water on the ocean floor depends on various factors, including temperature, salinity, and overall ocean circulation patterns. Ultimately, it is part of a complex system that can lead to gradual mixing and eventual return to the surface.
What else can I help you with?
Is cold ocean water more dense than water water?
more dense
Where is the ocean most dense?
The ocean is most dense towards the bottom of the sea. As the water in the ocean gets colder it gets more dense.
What causes water near the ocean floor to move from poles to equator?
Water near the ocean floor moves from the poles to the equator primarily due to thermohaline circulation, which is driven by differences in temperature and salinity. Cold, dense water at the poles sinks and flows towards the equator, while warmer, less dense water rises and moves poleward at the surface. This global conveyor belt of ocean currents plays a crucial role in regulating climate and distributing heat across the planet. Additionally, the Coriolis effect influences the direction of these currents as they move along the ocean floor.
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 ocean current?
Deep ocean currents are created by differences in water density. Cold or salty water is more dense and sinks, whereas warm or less salty water is less dense and rises. In polar regions, much of the ocean water is tied up in ice sheets. The salt remains in the liquid water, so the water in these areas is very salty as well as very cold. This water is consequently very dense and sinks. It is replaced by water from lower latitudes. The deep, dense water then moves slowly across the ocean floor and eventually rises in warmer latitudes. These currents are connected, and are sometimes called the ocean "conveyor belt." One circuit can take 1000 years to complete0_O
What is more dense cold water or warm?
cold ocean water is more dense than warm water
What is the vertical section of the ocean from the surface to the ocean floor referred to as?
This section of the ocean from floor to surface is called the water column.
What is is the Antarctic bottom water how does it form?
Antarctic Bottom Water (ABW) is a dense, cold water mass that forms primarily around the Antarctic continental shelf, particularly in the Weddell Sea. It is created when sea ice forms, increasing the salinity and density of the surrounding water as the salt is expelled into the ocean. This dense water then sinks to the ocean floor and flows northward, contributing to global ocean circulation. ABW is crucial for regulating climate and transporting heat and nutrients in the deep ocean.
Why does the ocean water get saltier after evaporation?
If water is evaporated salt remain in the ocean.
Is water from a glacier more dense than ocean water?
The water from a melted glacier is less dense than the water of the seas.
What is ocean currents?
Deep ocean currents are created by differences in water density. Cold or salty water is more dense and sinks, whereas warm or less salty water is less dense and rises. In polar regions, much of the ocean water is tied up in ice sheets. The salt remains in the liquid water, so the water in these areas is very salty as well as very cold. This water is consequently very dense and sinks. It is replaced by water from lower latitudes. The deep, dense water then moves slowly across the ocean floor and eventually rises in warmer latitudes. These currents are connected, and are sometimes called the ocean "conveyor belt." One circuit can take 1000 years to complete0_O
How deep currents form and move in the ocean?
deep ocean currents form by the differences in the density of ocean water
