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Heat Transfer in Nature

In liquids and gases: convection

Water is a poor conductor. Yet a pan of water heats up fast. How?

A pan of water is warmed at the bottom.
Step 1 of 4
  1. A pan of water is warmed at the bottom.
  2. The warm water at the bottom rises.
  3. Cooler water from the top sinks to take its place.
  4. This goes round and round. Soon all the water is warm.

Moving water carries the heat to all of the pan.

Warm water takes up a little more room. It is lighter for its size, so it rises.

The new word

  • Convection — heat carried by a moving liquid or gas.

The rule

In a liquid or a gas, the warm part rises. The cooler part sinks to take its place. This is convection.

Air carries heat too

By day, cool air comes in from the sea.

A breeze is a gentle wind. By day, land heats faster than the sea. Warm air over land rises. Cool sea air moves in: a sea breeze. At night the air moves the other way: a land breeze.

Watch out!

Warming a water tank from the top does not mix the water. Warm water is lighter for its size, so it stays on top. The bottom stays cold for a long time.

Now try it. Slide the heater up the tank. Count the warm layers.

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This track

  1. 0 Start here
  2. 1 Heat and temperature are different
  3. 2 Heat moves from hot to cold
  4. 3 Through a solid: conduction
  5. 4 In liquids and gases: convection
  6. 5 Across empty space: radiation
  7. 6 Three ways, every day
  8. 7 Checkpoint: how heat moves
  9. 8 The water cycle
  10. 9 Water seeping into the ground
  11. 10 Sea breeze and land breeze
  12. 11 Ice stupas
  13. 12 Checkpoint: water, breezes and ice
  14. 13 The big picture
  15. 14 Track quiz

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