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Convection

Thermal physics · IGCSE Physics

Convection — IGCSE Physics Notes

Exam years: 2025–2027 Topic: Thermal physics Lesson 17 of 48

Convection

Convection is the transfer of heat in liquids and gases through the movement of the fluid itself.

Key Features
  • Occurs only in liquids and gases.
  • Heat is transferred by circulating currents within the fluid.
  • Hotter, less dense regions rise; cooler, denser regions sink, creating a convection current.

Explanation in Terms of Density Changes

When a fluid is heated, its particles move faster and spread apart, causing the fluid to expand. Because the mass remains the same, the density decreases, making the warmer region rise upward. Cooler, denser fluid then sinks to take its place, establishing a continuous cycle.

Summary Process
  • Heated fluid expands → less dense → rises upward.
  • Cooler fluid sinks to replace it → more dense.
  • This creates a continuous convection current.
Convection Currents

Convection currents efficiently transfer thermal energy from hotter to cooler parts of a fluid. This is why stirring is not required when heating liquids; heat spreads naturally by convection.

Examples of Convection in Daily Life

1. Sea Breeze (Daytime)

During the day, the land heats up faster than the sea. The air above the land becomes hot and less dense, so it rises. Cooler air from above the sea moves in to take its place, forming a sea breeze — air moving from sea to land.

2. Land Breeze (Nighttime)

At night, the land cools faster than the sea. The air above the warmer sea becomes hotter and less dense, so it rises. Cooler air from the land moves out to take its place, forming a land breeze — air moving from land to sea.

Situation Hot Region Direction of Air Movement Breeze Name
Daytime Land hotter than sea From sea to land Sea breeze
Nighttime Sea hotter than land From land to sea Land breeze
Exam Tip

In convection, heat transfer occurs because the particles move. This is different from conduction, where particles only vibrate.

Key Points to Remember
  • Convection cannot occur in solids or in a vacuum.
  • Heating a fluid from below produces stable convection currents.
  • Applications: room heaters, sea and land breezes, boiling water.

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