Atmospheric Refraction
Atmospheric refraction is the bending of light by layers of air in the Earth's atmosphere because the air density changes with height.
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Student-friendly explanation
The atmosphere is not uniform. Near the ground, air is denser, and higher up, air is less dense. Light bends gradually as it passes through these layers. This is why some sky objects appear shifted from their actual positions and why some sunrise and sunset effects occur.
How to write this in exams
- 1
Start with the exact idea
Atmospheric refraction is the bending of light by layers of air in the Earth's atmosphere because the air density changes with height.
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Then show how to use it
1. State that atmospheric layers have different densities. 2. Explain that light bends gradually as it passes through them. 3. Relate this to the apparent position of the Sun. 4. Mention advanced sunrise or delayed sunset as examples.
- 3
Add one concrete example
The Sun may be seen slightly before actual sunrise and a little after actual sunset because its light bends through the atmosphere.
- 4
Avoid this incomplete answer
A common wrong answer is that the Sun moves upward quickly at sunrise. That is wrong because the effect is due to bending of light, not Sun motion.
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Why can the Sun be seen slightly before actual sunrise?
The Sun is seen slightly before actual sunrise because its light bends while passing through layers of the atmosphere. This atmospheric refraction makes the Sun appear higher than its actual position.
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