Sun Exposure Seat Finder
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Calculate the length of a shadow for any height, location, date, and time. Includes an interactive visual builder designed for children, physics students, and educational science experiments.
Select a historical or modern location to load its coordinates.
Enter your height or the object's height in centimeters.
4.76 ft
Moderate height (Afternoon)
Shadow is shorter than height
As the sun gets higher in the sky, the angle increases and your shadow becomes shorter. At noon, the sun is at its highest point, making your shadow the shortest of the day.
Have you ever wondered why your shadow looks extremely tall in the evening but almost disappears at noon? The length of a shadow is determined by the geographic relationship between an object, the ground, and the position of the sun. Using a shadow length calculator allows students, children, and scientists to compute the exact dimensions of a shadow cast by any object at any coordinates on Earth.
If you are interested in mapping sunlight for other purposes, you can use our Golden Hour Calculator to find the best photography times, or use the Sun Exposure Seat Finder to select the best shaded seat on a bus. For solar energy systems, our Solar Panel Angle Calculator calculates the optimal tilt angle based on your location's latitude.
The math that determines shadow length relies on solar elevation angle (altitude). The solar elevation angle measures how high the sun is relative to the horizon plane, ranging from 0 degrees (at sunrise or sunset) to 90 degrees (when the sun is directly overhead at the zenith). By applying basic right-angle trigonometry, we can convert the height of an object and the sun's angle into a precise horizontal measurement.
This tool processes coordinates, dates, and times entirely client-side using JavaScript. Your precise location and browser data remain completely private and are never transmitted to any external server.
Calculations for a shadow length calculator are based on a right-angled triangle formed by the object (the vertical side), the ground shadow (the horizontal side), and the incoming solar rays (the hypotenuse).
Where:
Let's look at an example. If a child stands 150 cm tall and the solar elevation is 45 degrees, we calculate:
Shadow Length = 150 / tan(45°) = 150 / 1 = 150 cm
When the solar elevation is exactly 45 degrees, the shadow length is equal to the object's height. If the sun is higher in the sky (e.g. 60 degrees), the tangent value is greater than 1, making the shadow shorter than the object. If the sun is lower in the sky (e.g. 20 degrees), the tangent value is less than 1, making the shadow much longer than the height.
The study of shadows holds a historic place in scientific history. Around 240 BC, the Greek polymath Eratosthenes utilized vertical columns and solar shadows to calculate the circumference of the Earth with remarkable accuracy.
Eratosthenes heard reports that at solar noon on the summer solstice in the southern city of Syene (modern Aswan, Egypt), the sun shone directly down a deep water well, casting no shadows. This meant the sun was directly overhead at an elevation angle of 90 degrees.
Simultaneously in Alexandria, located directly north, he measured the shadow cast by a vertical pillar (obelisk) at solar noon. Using the height of the column and the shadow length, he calculated that the sun's rays hit the column at an angle of 7.2 degrees from the vertical.
Knowing that 7.2 degrees represents exactly 1/50th of a full 360-degree sphere, Eratosthenes reasoned that the distance between Alexandria and Syene must be 1/50th of the Earth's circumference. By multiplying the estimated distance by 50, he calculated a total circumference of approximately 250,000 stadia (about 40,000 kilometers), which is incredibly close to the actual modern value of 40,075 kilometers.
Shadow calculations offer a hands-on, visual way to introduce children and physics students to astronomical mechanics and basic geometry:
The length of a shadow is calculated using basic trigonometry: Shadow Length = Height / tan(α), where Height is the physical height of the object or person, and α (alpha) is the solar elevation angle (altitude) above the horizon. If the sun is directly overhead (90° elevation), the shadow length is zero. If the elevation angle is 0° (sunrise or sunset), the shadow is theoretically infinitely long.
In the early morning and late evening, the sun is positioned low in the sky, resulting in a small solar elevation angle. Tracing the sun's rays mathematically shows that low-angle rays must travel much farther along the ground before hitting the surface, creating longer shadows. At solar noon, the sun reaches its highest daily point, casting the shortest shadows.
Around 240 BC, Greek mathematician Eratosthenes observed that at solar noon on the summer solstice, the sun was directly overhead in Syene (modern Aswan, Egypt) and cast no shadow down a deep well. Simultaneously in Alexandria, he measured the shadow angle of a vertical column to be about 7.2 degrees (1/50th of a full 360° circle). By multiplying the distance between Alexandria and Syene by 50, he accurately estimated the Earth's circumference.
At night, the solar elevation angle is negative, indicating the sun has set below the horizon. The calculator identifies this state and displays that no direct solar shadow is cast, showing a nighttime illustration instead.
The calculator supports both Metric units (meters and centimeters) and Imperial units (feet and inches) for the height input. The calculated shadow length is dynamically converted and displayed in the selected system for easy reference in classroom physics experiments.
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