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Year 10 Earth and space

The universe from the big bang to today and the evidence that it is expanding, then Earth's energy balance: sunlight absorbed and reflected, energy flowing between the spheres, and the greenhouse effect. Concept tutorials with a timeline of the universe, expanding space, and a live energy-balance model.

Start1. How did the universe begin?

The big bang

The big bang model and redshift as evidence for expansion (AC9S10U03).

1How did the universe begin?Not started

The big bang theory: space, time, matter and energy began about 13.8 billion years ago in an extremely hot, dense state, and the universe has expanded and cooled ever since: from particles to atoms, stars, galaxies and planets.

  1. Engage: an explosion?
  2. Explore: 13.8 billion years
  3. Explain: the model › Order
  4. Explain: the model › Atoms
  5. Explain: the model › Your atoms
  6. Explain: the model › Expanding and cooling
  7. Explain: the model › In your own words
  8. Evaluate: look back
Start lesson
2How do we know the universe is expanding?Not started

Light from distant galaxies is redshifted: shifted to longer wavelengths, so they are moving away. Farther galaxies move away faster (Hubble's law), exactly what an expanding universe predicts, from any galaxy. Run backwards, everything was once together: evidence for the big bang.

  1. Engage: the centre?
  2. Explore: stretch space › Reading a spectrum
  3. Explore: stretch space › Stretch space
  4. Explain: redshift and Hubble's law › Redshift
  5. Explain: redshift and Hubble's law › The pattern
  6. Explain: redshift and Hubble's law › Back in time
  7. Explain: redshift and Hubble's law › In your own words
  8. Evaluate: look back
Start lesson
6Quick check: scale, the cosmic glow and the evidence OptionalNot started

Earth's energy balance

Sunlight in, energy balance between the spheres, and the greenhouse effect (AC9S10U04).

3Where does the sunlight go?Not started

The sun is Earth's main energy source. Some sunlight is reflected straight back to space and the rest is absorbed and warms the planet. How much is reflected (the albedo) depends on the surface: ice reflects most, oceans and forests absorb most.

  1. Engage: does all sunlight warm the Earth?
  2. Explore: change the surfaces
  3. Explain: absorbed and reflected › Reflect or absorb
  4. Explain: absorbed and reflected › Melting ice
  5. Explain: absorbed and reflected › Light or dark
  6. Explain: absorbed and reflected › In your own words
  7. Evaluate: look back
Start lesson
4What keeps Earth's temperature steady?Not started

Earth is in energy balance when the energy it absorbs from the sun equals the energy it gives off to space as infrared. Energy moves between the spheres by radiation, conduction and convection, and the oceans store heat. Upset the balance and Earth warms or cools until it is restored.

  1. Engage: why doesn't Earth keep heating up?
  2. Explore: upset the balance
  3. Explain: energy in, energy out › Balance
  4. Explain: energy in, energy out › Restored
  5. Explain: energy in, energy out › How energy moves
  6. Explain: energy in, energy out › In your own words
  7. Elaborate: the ocean as a store
  8. Evaluate: look back
Start lesson
5How do greenhouse gases warm the Earth?Not started

Earth gives off infrared. Greenhouse gases (water vapour, CO₂, methane, nitrous oxide) absorb some of it and send part back down, slowing the energy going out. Without them Earth would average about −18 °C. Adding more upsets the balance, and Earth warms until it is restored.

  1. Engage: what do greenhouse gases do?
  2. Explore: remove them, then add more › No greenhouse gases
  3. Explore: remove them, then add more › Double the CO₂
  4. Explain: natural and enhanced › Which flow
  5. Explain: natural and enhanced › Natural or enhanced
  6. Explain: natural and enhanced › Rise and level off
  7. Explain: natural and enhanced › In your own words
  8. Evaluate: look back
Start lesson
7Quick check: causes, evidence and responses OptionalNot started

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