Rocket lines up two glasses on the Station Rooftop table. One holds ice and cold water. The other holds plain water from the tap.
"Same room, same air," he says. "If the air is full of water, both glasses should sweat."
Raven starts a timer. "What do you notice after five minutes?"
Rocket leans in. "The icy one is already fogging up. The other one is dry."
Nova hovers between them. "Same air touched both glasses," she says. "What was different about the air that touched the cold one?"
"It got cold," Rocket says slowly. "Cold enough to let the water out."
Raven writes a new word at the top of the data sheet: dew point.
You will chill one glass with ice and leave another at room temperature. Then you will watch which one collects water from the air, and how much.
This is a fair test. The only thing that changes between the two glasses is the temperature.
The National Weather Service uses this same demonstration in its JetStream lessons.
| Time | Icy glass | Room temperature glass | Room feels (dry, normal, humid) |
|---|---|---|---|
| 5 minutes | |||
| 10 minutes | |||
| 20 minutes | |||
| 30 minutes |
Air touching the icy glass cools below its dew point. The water vapor in that air condenses onto the glass as liquid drops.
The dew point is the temperature air must cool to before it is saturated and cannot hold any more vapor.
The room temperature glass does not cool the air, so nothing condenses on it.
How much water collects depends on the humidity. The more water vapor the air holds, the more can condense.
On a humid day, the icy glass drips. On a very dry day, it may only fog lightly.
| What the lab shows | True or false? |
|---|---|
| The water on the outside of the icy glass came from the air. | ? |
| Both glasses collected the same amount of water. | ? |
| Air touching the icy glass cooled below its dew point. | ? |
| More humid air leaves more water on the glass. | ? |
Great lab work. Tomorrow you will read real dew point numbers from a National Weather Service office.