Find Out Why the Ocean is in Motion!
You probably know that water never stays still. But did you know that there is something called the global “ocean conveyor belt” that moves massive amounts of water from one ocean to another? These water currents are essential for mixing and transporting nutrients and oxygen, and play a critical role in our climate. This is because they move warm and cold water over very long distances, which affects the temperature of the landmasses that border the ocean. The Gulf Stream, for example, is one warm current from the Gulf of Mexico that moves into the North Atlantic Ocean and makes the climate in Europe much warmer. Do you want to know what causes the “ocean conveyer belt”? It is pretty simple: Differences in water density! Try this activity to learn more!
This activity is not appropriate for use as a science fair project. Good science fair projects have a stronger focus on controlling variables, taking accurate measurements, and analyzing data. To find a science fair project that is just right for you, browse our library of over 1,200 Science Fair Project Ideas or use the Topic Selection Wizard to get a personalized project recommendation.
There is a lot of water movement in the ocean. The most obvious examples are the waves and ripples on the water’s surface that are generated by wind, or ocean currents due to tides. It turns out, however, that water can also be moved without wind or tides, which is what happens in the deep ocean. There, currents are set in motion by variations in water density caused by differences in temperature and salinity, a process called convection.
The density of a substance is defined by its mass per volume; one liter of water, for example, does not weigh the same as one liter of oil. The lighter liquid will float on top, while the heavier liquid will sink to the bottom. The density of water varies with temperature. When water is heated, it will expand and therefore increase in volume. This means that its mass per volume will decrease and it becomes less dense. Thus, warm water is generally less dense than cold water. Another factor that affects water density is salinity, which is the amount of salt in ocean water. More salt makes water heavier, and therefore denser.
These two factors, temperature and salinity, are the main driving forces behind the global ocean conveyor belt, which is a huge water circulation system in the deep ocean that moves water around the globe. Currents begin near the pole in the North Atlantic where the surface of the ocean gets cooled by the arctic temperatures. As sea ice forms, salt stays behind and the water becomes saltier. This water is now denser, and will sink to the bottom of the ocean floor. This creates a current, as surface water has to move in to replace the sinking water. The cold water moves all the way to Antarctica, and then to the Indian and Pacific Oceans. Once the water reaches warmer regions, it warms up, becomes less dense, and rises to the surface. Eventually, it finds its way back to the North Atlantic where the whole cycle begins again. In this activity, you will demonstrate how temperature affects water movement and water density, and create your own little ocean currents in a glass!
Extra: In this experiment, you have shown that differences in temperature drive water movement. What happens if you have no temperature gradient? Repeat the same experiment, but this time do not heat or cool the water in the cups—keep them at the same temperature. Do you see any water movement happening when you remove the plastic strip? Why or why not?
Extra: Can you find a way to demonstrate how salinity affects water density and water movement? Add salt to one of the cups to create a salinity gradient and repeat the experiment. Does the salty water float or sink? Can you create water movement with a salt gradient?
Extra: Instead of demonstrating that warm water floats on top of cold water, show how cold water sinks to the bottom and add the food coloring to the cold water instead of the warm water. Then place the cold water on top of the warm water and vice-versa. Do you see water movement in both directions, or only in one?
Extra: How does the temperature gradient affect the water mixing? Add a third experiment, in which the temperature difference between the warm and cold water is different from your previous experiment. What changes if you have a higher versus a lower temperature difference between the hot and cold water?
Observations and Results
Were you able to make your water move to float and sink? When you add the food coloring to the hot water and place the cold water on top of the hot water, initially nothing should have happened as the plastic strip should have still covered the hole of the CD, preventing the water from mixing between the cups. However, as soon as you remove the plastic strips, the dyed warm water will shoot through the CD hole and mix with the cold water above.
This water movement is driven by convection: the movement of water due to differences in temperature. As the warm water is lighter than cold water and wants to expand, it moves into the upper cup through the hole. After about 10 minutes, the mixing should almost be completed, and the color of the water should be similar in both cups. At the same time, the temperature in both cups should have changed significantly. In the beginning, you should have measured a large temperature difference, but at the end, both temperatures should have been similar. As the water was mixing, heat exchange occurred, which means that the warm water was heating up the cold water. If you tried the extra activity with a higher or lower temperature difference between both cups, you should have noticed that the mixing of water happens faster when the temperature difference is larger. When you have no temperature gradient at all, no significant mixing will happen within 10 minutes.
If you reverse the experiment and have the warm water on top of the cold water, you should have seen that the water did not mix between the cups. This is because warm water is lighter, or less dense, than the cold water, which is why it wants to remain on top of the cold water. The same is true for salty versus non-salty water. Salty water will always sink to the bottom, as it is denser than non-salty water—exactly how it does in the real ocean!
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Svenja Lohner, PhD, Science Buddies
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Convection, temperature, density
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