Ferris Wheels are large amusement-park rides that carry us high up to provide an unrivaled view of the surroundings. They do no useful work, and are typically driven by one or more electric motors at the base. Around and around they go in a steady, ceaseless motion. Although typical Ferris Wheels do no useful work, Ferris Wheels could be repurposed as follows.
High on a cliff is a remote resort with no road access. Although people periodically ascend to or descend from the remote resort by other means, a steady stream of heat, fresh water, and food must be continuously supplied to the remote resort. A Ferris Wheel is mounted at the base of the cliff near a geothermal vent that provides a constant source of hot air. Nearby springs provide a supply of fresh water. Food is shipped in from a nearby town.
The gondolas of the Ferris Wheel have envelopes attached above them. As the gondolas pass over the geothermal vent, hot air rises, filling the envelope and pulling the gondolas upward. Fresh water and food are continuously loaded onto the gondolas as they pass by at the base of the cliff. At the top of the cliff, the hot air is removed from the balloons and used to heat the resort. The fresh water and food on the gondolas are automatically removed and replaced with waste water.
The hot air in the balloons pulls the water and food upward to the resort. Waste water from the resort loaded on the descending side of the Ferris Wheel pull it downwards. The combined upward and downward forces keep the Ferris Wheel constantly turning, providing a never-ending stream of heat, food, and water to the remote resort. The key driving element is that the air is more buoyant on one side of the wheel than on the other: the buoyancy difference drives the Ferris Wheel.
The natural world also has mechanisms for continually transporting energy, oxygen, and nutrients to places where they’re needed, because a regular flow of energy, fresh water, and nutrients is needed for healthy life. Most lakes turn over twice each year because water is denser at 4°C than at temperatures higher or lower than this. Buoyancy-driven lake turnover twice/year brings oxygen from the surface to the bottom, so that life is sustained throughout the entire depths of the lake.
The oceans contain similar mechanisms of constant motion and change. Referred to by some as “Ocean conveyor systems”, the familiar Gulf Stream is but one part of an oceanic river that moves oxygen, energy, and nutrients from one place to another. First discovered by Ponce de Leon in 1513, the Gulf Stream was first charted by Benjamin Franklin in the early 1770’s, as depicted in this chart he made (see Fig. 1).
Figure 1. NOAA. “Who First Charted the Gulf Stream?” National Ocean Service website, accessed on 9/18/21 (NOAA).
By now scientists have given us a more complete picture of this oceanic river system, referred to generically as the Meridional Overturning Circulation (MOC), shown in Fig. 2. The Atlantic branch of the MOC is the Atlantic Meridional Overturning Circulation (AMOC), of which the Gulf Stream is a part.
Figure 2. Illustration from the Met Office showing the Meridional Overturning Circulation (MOC). The Gulf Stream is the part in the upper left, which flows from Florida in the USA, northeast to Europe. Reproduced from the Met Office, “What is the Atlantic Meridional Overturning Circulation?” (Met Office).
Whereas in lakes it is primarily density changes that drive the bi-annual turnover, in the oceans it is primarily a combination of density changes and winds that drive the large ocean currents. In one part of the ocean denser water sinks, driving the flow downwards, whereas in other parts of the ocean strong surface winds draw water up from the deep ocean. This combined sinking on one end and upwelling in another part keeps these ocean rivers constantly flowing.
This continual motion distributes oxygen, energy, and nutrients throughout the ocean system, benefitting both aquatic and terrestrial life. By distributing energy from the Equatorial regions up to the northern latitudes, the Gulf Stream makes life in Europe more bearable than it would be otherwise.
Europe is like a remote resort high up in the Northern Hemisphere. People may periodically come and go to Europe by other means, but the steady flow of energy and nutrients needed to make life bearable in Europe comes largely from these ocean rivers. Without the Gulf Stream and other similar ocean currents, life on Earth would be much different.
On the driving processes of the Atlantic meridional overturning circulation (AGU Publication)
Posted by Evan on Monday, 27 September, 2021
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