At the edge of the canopy
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.
Dark line: measured reference shadow. Brown dot: Sun direction. The leafy tree provides context.
Change the light
Height above the horizon
Clockwise from north: N 0° · E 90° · S 180° · W 270°
- Shadow length
- 5.00 m
- Shadow bearing
- 315°
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).
This model measures the shadow of a marked point on an upright 5 m reference beside a tree. It assumes parallel sunlight and level ground. It does not compute the canopy’s outline, soft shadow edges, slopes, weather, or atmospheric refraction. The controls are independent experiments, not a daily or seasonal solar path.
- NOAA: azimuth and elevation definitions
- NASA: shadow geometry, page 4 (local geometry only; the document concerns lunar lighting)
- NOAA: observing shadows