Why does a tree’s shadow move and change length?
Move the Sun and watch the shadow of a marked point 5 metres above level ground.
01 / Height above the horizon
A light ray meets level ground
Fixed scale. The measured shadow belongs to the marked pole beside the tree.
10° near the horizon → 80° high in the sky
02 / Around the horizon
Look down on the shadow
Fixed scale · the outer ring is 30 m from the reference. Pale dot: Sun direction. Gold line: reference shadow.
Shadow bearing
Clockwise from north: N 0° · E 90° · S 180° · W 270°
Follow the light to the ground
The shadow points away from the Sun. Lower sunlight meets the ground farther from the reference, making a longer shadow. Moving the Sun around the horizon changes the shadow’s direction. At a fixed elevation, that rotation does not change its length.
Geometry, assumptions, and sources
In the right triangle, tan(elevation) = height ÷ shadow length. Rearranging gives shadow length = height ÷ tan(elevation).
We model the marked point on an upright 5 m pole beside a tree, using parallel sunlight and level ground. This does not compute a canopy outline, soft edges, slopes, weather, or atmospheric refraction. The two controls are independent experiments, not a real daily or seasonal solar path.
- NOAA: azimuth and elevation definitions
- NASA: local shadow geometry, page 4 (a lunar-lighting document; only the geometry is used)
- NOAA: observing shadows