Fog fills the field at sunrise. By lunch it's gone. Where did it go?

It looks like a soft cloud rolled in… then quietly rolled away. But did it really travel anywhere? Let's mess with the air and find out what fog actually is.

1Two things about air and water

Air secretly carries water — and there's a limit

You only need two ideas. Watch each one:

Air carries invisible water

Mixed into the air all around you is water you can't see. It's not droplets and it's not steam — it's water spread out so finely it's completely invisible. We call that invisible water vapor.

Warm air carries more than cool air

Air can only hold so much invisible water — and the limit changes with temperature. Warm air has lots of room. Cool air has very little. Same air, different limit.

2Roomy air vs crowded air

The same water, two very different rooms

Picture the air as a room for water. The temperature decides how big the room is:

Warm air

The roomy carrier

Lots of space, so all the water spreads out and stays invisible. The air looks perfectly clear.

Cool air

The crowded carrier

Hardly any room. The water that won't fit gets squeezed out into tiny visible droplets — that's fog.

3Your turn — fill the air with water

Pour invisible water in until the air can't hold it

Here the temperature stays the same. Slide to add more and more invisible water. Watch the air's water-room fill up — and see what happens when you pour in more than it can hold.

The air's water-room: room to spare
Invisible water you've addeda little
BONE DRYSOAKING

4Now run a whole morning

Same water all night. The sun comes up. Watch the fog. ☀️

This time the amount of water never changes — not a single drop comes or goes. The only thing you move is the temperature, from a cold night into a warming morning. Guess first, then drive the sun.

Guess before you drive the sun

The sun warms up the foggy morning air. Where does the fog go?