← Year 10 Earth and space

Year 10 Earth and space: recap

Answer each question in your head or on paper first, then check it.

The big bang

1. How did the universe begin?

Try firstOutline three stages of the universe after the big bang.

Check your answer

For example: the first nuclei of hydrogen and helium (3 minutes), atoms forming and light set free (380 000 years), the first stars (about 200 million years), galaxies (about 1 billion years).

The big bang theory: space, time, matter and energy began about 13.8 billion years ago in an extremely hot, dense state; the universe has expanded and cooled since, forming nuclei, atoms, stars and galaxies. Heavier elements were made in stars.

A patch of the universe soon after the big bang: extremely hot and dense.
A patch of the universe soon after the big bang: extremely hot and dense.
The big bang · Sound on for the voiceover
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2. How do we know the universe is expanding?

Try firstWhat does redshift show, and how does it support the big bang?

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Galaxies are moving away, farther ones faster: the universe is expanding. Run backwards, everything was once together in a hot, dense state.

Redshift: light from distant galaxies is stretched to longer wavelengths, so they are moving away. Farther galaxies move faster (Hubble's law): an expanding universe with no centre. Run backwards, it began together: the big bang.

A field of galaxies. When space expands, every galaxy moves away from every other, farther ones faster.
A field of galaxies. When space expands, every galaxy moves away from every other, farther ones faster.
An expanding universe · Sound on for the voiceover
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Earth's energy balance

3. Where does the sunlight go?

Try firstWhy does replacing sea ice with open ocean warm the area?

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Ice reflects most sunlight (about 80%); dark ocean absorbs most (reflects about 6%), so more energy is absorbed.

Sunlight is Earth's energy input. Some is reflected (the albedo, about 30% overall) and the rest absorbed. Bright surfaces reflect most; dark surfaces absorb most.

Surfaces under the sun: bright ones (ice) reflect most sunlight; dark ones (ocean, forest) absorb most.
Surfaces under the sun: bright ones (ice) reflect most sunlight; dark ones (ocean, forest) absorb most.
Where sunlight goes · Sound on for the voiceover
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4. What keeps Earth's temperature steady?

Try firstWhat is energy balance, and what happens if more energy comes in than goes out?

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Energy in equals energy out over time. If more comes in, Earth warms until it gives off enough extra infrared to balance again.

Energy balance: absorbed sunlight = infrared given off to space. If in exceeds out, Earth warms until out catches up. Energy moves between spheres by radiation, conduction and convection; the oceans store and carry heat.

Sunlight in, some reflected, the rest absorbed; infrared given off to space.
Sunlight in, some reflected, the rest absorbed; infrared given off to space.
Energy balance · Sound on for the voiceover
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5. How do greenhouse gases warm the Earth?

Try firstExplain how adding CO₂ warms the Earth.

Check your answer

CO₂ absorbs infrared from the surface and sends some back down, so less energy escapes; energy in exceeds energy out, and Earth warms until it gives off enough to balance again.

Greenhouse gases absorb outgoing infrared and send some back down, slowing energy loss. The natural effect keeps Earth about 15 °C (not −18 °C); the enhanced effect from extra greenhouse gases upsets the balance, so Earth warms. Not the ozone hole.

Sunlight in; infrared from the surface, part absorbed by greenhouse gases and sent back down.
Sunlight in; infrared from the surface, part absorbed by greenhouse gases and sent back down.
The greenhouse effect · Sound on for the voiceover
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