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Daylight

physical science Maturity 7-9 Next article →

Daylight is the total combination of all direct and indirect sunlight during the daytime. It is more than just the rays hitting us straight from the sun. Daylight includes direct sunlight and diffuse sky radiation. Diffuse sky radiation is light that is scattered throughout the sky. It also includes light reflected by Earth and terrestrial objects. These objects include landforms and buildings. Even though moonlight is reflected sunlight, it is not considered daylight. Daylight is defined by the Sun being above the local horizon.

Daylight
Daylight

How daylight reaches us depends on the Earth's atmosphere. The atmosphere performs a process called refraction. Refraction is when the air bends the light rays. This bending allows light to reach parts of the Earth even when the Sun is below the horizon. Because of this refraction, more than 50% of the Earth receives daylight at any given time. This means daylight is a global phenomenon that covers more than half our planet constantly.

Daylight
Daylight

Scientists measure the brightness of this light using a unit called lux. Outdoor illuminance varies greatly depending on the weather and the time of day. At its brightest, direct sunlight at noon can reach 120,000 lux. This level of light is so strong it may cause eye pain. Bright sunlight is slightly less, measured at 111,000 lux. Another specific measurement is the AM 1.5 global solar spectrum. This sunlight measures 109,880 lux or 1,000.4 W/m2.

Daylight
Daylight

Other conditions create much lower levels of light. If you are in the shade at midday, you might see 20,000 lux. This is light illuminated by the entire clear blue sky. On a typical overcast day at midday, the light drops to 1,000 to 2,000 lux. A clear day during sunrise or sunset provides about 400 lux of ambient illumination. Even more extreme conditions exist. Thick storm clouds can drop the light to less than 200 lux. In the most extreme cases of thick clouds, it may be less than 5 lux. This can be so dark that shadows from distant street lights become visible.

Daylight
Daylight

Sometimes, unusual circumstances can make the day much darker than normal. A solar eclipse can cause a sudden drop in light. High levels of atmospheric particulates can also block the sun. Particulates are tiny pieces of matter floating in the air. These include dust, volcanic ash, and smoke. There was even a historical event called New England's Dark Day caused by smoke. In these extreme cases, the light can fall below 1 lux.

Daylight
Daylight

We can understand the power of daylight by comparing it to nighttime illuminance. Nighttime is significantly dimmer than any daylight condition. Moonlight on a clear night sky is less than 1 lux. A full Moon on a clear night is only 0.25 lux. A quarter Moon provides only 0.01 lux. Starlight and airglow on a moonless night are even lower, at 0.0002 lux. If you exclude airglow, starlight is 0.00014 lux. Even the brightest planet, Venus, is only 0.0001 lux on a clear night.

Daylight
Daylight

Daylight is a complex system of light and atmosphere. It connects the movement of our planet to the physics of light. The way light bends and scatters determines how we see our world. It affects everything from how much energy we receive to how we see shadows. Understanding these levels of lux helps scientists study the atmosphere and the sun. It also helps us understand the relationship between the Earth and other objects in our solar system.

Daylight
Daylight
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