{[ promptMessage ]}

Bookmark it

{[ promptMessage ]}

How Ocean Currents Work

How Ocean Currents Work - Deep Ocean Currents(Global...

Info iconThis preview shows pages 1–3. Sign up to view the full content.

View Full Document Right Arrow Icon
Deep Ocean Currents (Global Conveyor Belt) Invisible to us terrestrial creatures, an underwater current circles the globe with a force 16 times as strong as all the world's rivers combined [source: NOAA: "Ocean" ]. This deep- water current is known as theglobal conveyor belt and is driven by density
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full Document Right Arrow Icon
differences in the water. Water movements driven by differences in density are also known asthermohaline circulation because water density depends on its temperature (thermo) and salinity (haline). Density refers to an object's mass per unit volume, or how compact it is. A heavy, compact bowling ball is obviously going to be denser than an air-filled beach ball. With water, colder and saltier equals denser. At the earth's poles, when water freezes, the salt doesn't necessarily freeze with it, so a large volume of dense cold, salt water is left behind. When this dense water sinks to the ocean floor, more water moves in to replace it, creating a current. The new water also gets cold and sinks, continuing the cycle. Incredibly, this process drives a current of water around the globe. The global conveyor belt The global conveyor belt begins with the cold water near the North Pole and heads south between South America and Africa toward Antarctica, partly directed by the landmasses it encounters. In Antarctica, it gets recharged with more cold water and then splits in two directions -- one section heads to the Indian Ocean and the other to the Pacific Ocean. As the two sections near the equator, they warm up and rise to the surface in what you may remember as upwelling. When they can't go any farther, the two sections loop back to the South Atlantic Ocean and finally back to the North Atlantic Ocean, where the cycle starts again. The global conveyor belt moves much more slowly than surface currents -- a few centimeters per second, compared to tens or hundreds of centimeters per second. Scientists estimate that it takes one section of the belt 1,000 years to complete one full circuit of the globe. However slow it is, though, it moves a vast amount of water -- more than 100 times the flow of the Amazon River. [source: NOAA: "Currents"]. Cinching Our Belt? Many scientists fear that global warming could affect the global conveyor belt. If global warming leads to increased rain, as some believe it might, the added fresh water could decrease the salinity levels at the poles. Melting ice, another possibility of global warming, would also decrease salinity levels. Regardless of the means, the end scenario is the same: Warmer, less dense water won't be dense enough to sink, and the global conveyor belt could stop -- having far-reaching and devastating consequences [source: NOAA: "Currents"]. The global conveyor belt is crucial to the base of the world's food chain. As it transports water around the globe, it enriches carbon
Background image of page 2
Image of page 3
This is the end of the preview. Sign up to access the rest of the document.

{[ snackBarMessage ]}

Page1 / 9

How Ocean Currents Work - Deep Ocean Currents(Global...

This preview shows document pages 1 - 3. Sign up to view the full document.

View Full Document Right Arrow Icon bookmark
Ask a homework question - tutors are online