Rocket tapes a sheet of grid paper to the Sky Deck floor. Raven holds the flashlight straight above it.
"Count the squares in the bright spot," she says. Rocket counts fast. "Twelve!" He counts again, slowly. "Fourteen."
"Now the slant," Raven says. She tips the flashlight, same height. The light stretches across the paper.
Rocket counts. "Thirty-one squares. The same light on more than twice the paper."
Nova hovers above the grid. "What do you notice about how bright each square is now?"
"Dimmer," Rocket says. "Each square gets a smaller share."
"That is winter sunlight," Raven says. Nova hums. "Now write it down before you forget your numbers."
Today you measure the flashlight effect from Tuesday. The same light spread over more squares means less light per square.
This is the first of the two effects of the tilt: direct sunlight in summer, slanted sunlight in winter.
You will shine straight down, count squares, shine at a slant from the same height, and count again.
| Flashlight angle | Squares lit, trial 1 | Squares lit, trial 2 | Brightness of each square (bright, medium, dim) |
|---|---|---|---|
| Straight down | |||
| Slanted | |||
| Slanted more |
The flashlight gave off the same light every time. Only the angle changed. More squares lit meant less light for each square.
That is why slanted winter sunlight heats the ground less than direct summer sunlight. The energy is spread thinner.
The straight-down beam stands for the high summer Sun. The slanted beam stands for the low winter Sun.
What the model gets wrong: the real Sun lights a whole hemisphere at once, and its height changes slowly over months.
| What the model shows | True or false? |
|---|---|
| The slanted beam lit more squares. | ? |
| The slanted beam made each square brighter. | ? |
| The flashlight gave off more light when it was slanted. | ? |
| The straight-down beam stands for the summer Sun. | ? |
A model that measures. Tomorrow you read a Naval Observatory table of the longest and shortest days.