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Daylight

Natural light during the daytime From Wikipedia, the free encyclopedia

Daylight
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Daylight is the combination of all direct and indirect sunlight during the daytime. This includes direct sunlight, diffuse sky radiation, and (often) both of these reflected by Earth and terrestrial objects, like landforms and buildings. Sunlight scattered or reflected by astronomical objects is generally not considered daylight. Therefore, daylight excludes moonlight, despite it being reflected indirect sunlight.

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World map showing the areas of Earth receiving daylight around 13:00 UTC in April
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Definition

Daylight is present at a particular location, to some degree, whenever the Sun is above the local horizon. This is true for slightly more than 50% of the Earth at any given time, since the Earth's atmosphere refracts some sunlight even when the Sun is below the horizon.

Outdoor illuminance varies from 120,000 lux for direct sunlight at noon, which may cause eye pain, to less than 5 lux for thick storm clouds with the Sun at the horizon (even <1 lux for the most extreme case), which may make shadows from distant street lights visible. It may be darker under unusual circumstances like a solar eclipse or very high levels of atmospheric particulates, which include smoke (see New England's Dark Day), dust,[1] and volcanic ash.[2]

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Intensity in different conditions

More information Illuminance, Example ...

For comparison, nighttime illuminance levels are:

More information Illuminance, Example ...

For a table of approximate daylight intensity in the Solar System, see sunlight.

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See also

References

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