This demonstration will help you understand that the ocean is not like a swimming pool where the water is stationary, but more like a river with deep currents. You will be able to see how different types and densities of water behave and how this behaviour drives the whole system of ocean circulation.
(and preparation the day before)
Ocean circulation relies on different densities of water falling and rising. The density of water is affected by salinity and temperature. With this demonstration, you can understand how the ocean behaves more like a river with deep currents. This activity looks at just the impact of temperature, but you can experiment with salt as well, with some guidance in the 'Further ideas' section below.
Arctic water (blue)
Gulf Stream water (red)
The ocean is formed of layers of water of different temperatures that rise and fall helping to drive the ocean currents.
Try the activity again using some salty water. Just add a few teaspoons of salt to a glass of hot water and let it cool. You could add a different colour of food dye. Then use the straw pipette method described above to add it to the surface of your 'ocean'.
To do this activity like a scientist, you would need to make some predictions about how the different types of water might behave. These predictions are called hypotheses. Scientists then carry out a test to see whether their ideas are correct by observing. The next stage would be to think about what is causing the observed behaviour. Look at the 'Find out more' tab to learn about the science behind ocean circulation.
Part of:AXA Ocean Education
Brought to you by
Science | Ages 11-14
The Frozen Oceans Science resources introduce working scientifically concepts and skills to 11-14-year-olds through enquiry-based lessons which replicate work done by field scientists in the Arctic.