This activity is all about finding out how the ocean helps regulate the temperature of our planet, carrying hot and cold water around our oceans in a series of currents.
The equator is an imaginary line around the center of the earth. It is hotter at the equator because it gets more direct sunlight.
Polar ice caps are found in the arctic (at the top or north of the planet) and the antarctic (at the bottom or south of the planet).
When the ocean demo is set up you should see that the cold blue water sink and moves across the bottom of the tank towards the warmer water. The red water will rise and moves across the tank towards the colder water. This sets up a circular current.
This happens because cold water is denser and sinks to the bottom of the tank. Hot water is less dense so it rises up. As the cold water sinks, it pulls water in above it, allowing the hot water to come across. As the hot water rises it pulls water in from below it.
We see this happening in our oceans - warm water flows away from the equator to the ice caps where it cools down. Coldwater at the ice caps sinks and flows towards the equator, where it gets warmed up and begins to rise and flow away again. This is known as thermohaline circulation.
In 1992, a cargo ship container tumbled into the North Pacific, dumping 28,000 rubber ducks and other bath toys into the ocean. Over the next 25 years, the ducks washed up on several different continents, revealing a worldwide network of currents, that had been invisible!
During years 1 and 2, pupils should be taught to observe closely, using simple equipment
Pupils in years 3 and 4 should be given a range of scientific experiences to enable them to raise their own questions about the world around them.
KS3 Physics: Pupils should be taught about the seasons and the Earth’s tilt, day length at different times of year, in different hemispheres
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