Let go of an open balloon and the air rushes out; puncture a cycle tube and it hisses flat. In both, air moves — but which way, and why? That same simple rule, scaled up to the whole sky, is what makes the wind blow. Let's uncover it.
- Air moves from a region of high pressure to a region of low pressure.
- This moving air is what we call wind.
- So differences in air pressure cause winds to blow.
- A larger pressure difference gives a faster wind.
- By day, land heats faster than water, so air above land warms, rises and leaves low pressure.
- Higher-pressure air from the sea blows to the land — a sea breeze.
- At night, the water is warmer, so low pressure forms over the sea.
- Air then blows from land to sea — a land breeze.
In this Activity, we will join an inflated and an uninflated balloon to watch which way the air flows.
2. Inflate the second balloon and hold its mouth so no air escapes.
3. Insert the free end of the straw into the inflated balloon and tie it (no leaks).
4. Predict, then observe, what happens to the two balloons.
- Air flows to the empty balloon
- Stops when pressures equalise
- High pressure to low pressure
- The SI unit of pressure is N/m², also called the pascal (Pa).
- The practical unit of air pressure is the millibar (mb), equal to 100 Pa.
- Air pressure is also given in hectopascal (hPa), also equal to 100 Pa.
- Wind — Air moving from a region of high pressure to a region of low pressure.
- Sea breeze — The daytime wind that blows from the sea to the land.
- Land breeze — The night-time wind that blows from the land to the sea.