Cold Water Near the Poles Sinks and Flows

In the global conveyor belt cold water from the North Pole _____. Consequently air that is heated near the equator rises.

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The surface currents of the ocean.

. One big part of the oceans role is to soak up energy heat and distribute it more evenly around the Earth. Cold water from the poles pushes up warmer water. Then the cold water flows back along the ocean floor as a deep current.

-ends near the tip of Florida-is a dense cold water current. The ocean water near the poles sinks because it is denser than the water in the rest of the ocean. A carry warm water to the poles.

Cold water sinks near the North and South Poles. What makes ocean water more dense. They carry cold water from the poles toward the equator.

Water gets colder with depth because cold salty ocean water sinks to the bottom of the ocean basins below the less dense warmer water near the surface. Convection cells are set up with warm water moving along the surface to the poles. The cold water near the poles sinks and the surface water flows to take its place.

Water near the poles is colder and saltier than water near the equator. The ocean encloses a certain water activity creating the Global Conveyor Belt which is about the thermohaline circulation which is a system of currents. How cold currents create desiccating effect.

Flows directly into the Indian Ocean. In the Earths polar regions ocean water gets very cold forming sea ice. The oceans are mostly composed of warm salty water near the surface over cold less salty water in the ocean depths.

Cold water near the poles sinks and flows along ocean floors and water rises in warmer regions upwelling Upwelling occurs when winds push warm surface water away from the continent. Cold water near the poles sinks and flows parallel to the ocean bottom rising again in warmer regions. Cold water has a higher density than warm water.

What does deep ocean water do as it reaches the equator and warms. -happens when water sinks toward the ocean floor-happens when water rises to replace moving surface water-is caused by breaks or disruptions in a longshore current. At the same time cooler air over the poles sinks toward the ground.

Water chilled by colder temperatures at high latitudes contracts thus gets denser sinks and moves back toward the equator. In certain areas near the polar oceans the colder surface water also gets saltier due to. Sea ice is surprisingly essentially fresh water.

The ocean currents the movement of the ocean in the surface layer are driven mostly by the wind. And second cold water from the deep ocean comes up to the surface through a process called upwelling. Convection current of cold water flows from poles towards the equator.

Cold water from poles sinks and moves along the ocean floor in current. Cold-water ocean currents occur when the cold water at the poles sinks and slowly moves towards the equator. Two main factors affect the density of the ocean water.

Under the tropical sun water at the equator warms up. Water near the equator gets heated up whereas water near the poles is comparatively cold. The upward movement of warm air and the downward movement of cool air create air currents which move heat throughout the atmosphere from regions of sinking air to regions of rising air.

Formation of sea ice also helps to increase the density of water near Earths poles. So convection currents are produced by warm water flowing from equator towards the poles. Eventually the water rises to the surface and returns to the site of bottom water formation via surface currents red paths to start the cycle again By Robert Simmon NASA.

Fresh water near the Arctic sinks and moves toward the equator. The warm water flowing from the equator toward the poles helps warm the climate in North America and Europe. As a consequence the surrounding seawater gets saltier because when sea ice forms the salt is left behind.

As the cold water warms it starts to rise to the top and sends the warmer surface water back toward the poles. Surface Currents Because the air above a warm current is warm it can bring milder winters to places that would otherwise be significantly colder Gulf Stream and Britain. Cold salty water is dense and sinks to the bottom of the ocean while warm water is less dense and remains on the surface.

As the seawater gets saltier its density increases and it starts to sink. As sea water freezes salt is forced out of the ice in a process called brine exclusion. The excluded salt increases the salinity of the cold water immediately below the ice making it denser still.

B carry cold water to the equator. Why does the water near the poles sink. The water along the coast of California is cold for a couple of reasons.

At the frigid poles seawater cools down and sinks. The sinking and transport of cold salty water at. Warm-water currents travel out from the equator along the surface flowing towards the poles to replace the sinking cold water.

This cold water sinks and flows beneath the ocean surface toward the equator where it is warmed. The salty cold water near the poles sinks toward the. As water temperatures begin to decrease and salinity increase the water becomes denser and sinks.

Cold water also flows toward the equator getting warmer as it goes. Surface water is moved by winds. _____ flows in and out of all of Earths systems.

What causes ocean water near the equator to be warmer. First the California Current brings cold water from Alaska southward along the coast. Cold water currents begin near the poles and flow south as deep water currents.

C can move water away from a coastline. Surface water is moved by these. Basically the cold water tend to sink under the warm water which has more salt and more ability to absorb heat.

Deep currents move and mix water around the world. The warm water is lighter than cold water. These ocean currents are convection currents.

Currents move water from the equator to the poles. It moves toward equator. Cold dense water sinks in the Greenland and Weddell Seas and circulates over the seafloor into the Indian and Pacific Oceans blue paths.

Much of the water near the poles is frozen in icebergs and sea ice. A Water b Oxygen. So water from the deep ocean is sucked to the surface.

Water near the poles sinks and flows beneath warmer shallower water. The ocean does an excellent job of absorbing excess heat from the atmosphere. It then rises to replace the water that surface currents constantly carry toward the poles.

These two regions dont mix except in certain special areas.

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