Ice cores, archives of ancient air
Age 17 · Science
As snow piles up on Antarctica and Greenland, it compresses into ice and seals off tiny pockets of the air above it, so each layer holds a sample of the atmosphere from when it formed. By drilling cores more than 3 km deep and measuring the CO2 in those bubbles and the isotopes in the ice, scientists have reconstructed the climate of the last 800,000 years.
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In the picture
- Trapped air bubbles: real samples of past atmosphere, with their CO2 concentration
- Pale layers: yearly snowfall bands that let scientists count back in time near the top
- Deep, clear ice: older ice under huge pressure, holding air hundreds of thousands of years old
- Drill rig: brings up the core section by section from more than 3 km down
Examples
- Ice cubes from the freezer often have cloudy bubbles of air trapped as the water froze.
- Old snow at the bottom of a heap is packed harder and icier than fresh snow on top.
Key takeaways
- Over 800,000 years, CO2 swung between about 180 ppm in ice ages and 280–300 ppm in warm periods; today it is above 420 ppm.
- In ice cores, CO2 and temperature rise and fall together across glacial cycles.
Quiz: Ice cores, archives of ancient air (Age 17)
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Over the last 800,000 years, between which levels did atmospheric CO2 swing, according to ice cores?
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What do ice cores show about CO2 and temperature across glacial cycles?
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Why does each layer of polar ice hold a sample of the atmosphere from when it formed?
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