Difficulty: Medium
Correct Answer: Unequal heating of different parts of the atmosphere, producing layers with different densities and refractive indices
Explanation:
Introduction / Context:
Mirages are fascinating optical illusions often observed in deserts or on sun heated roads. A common type is the inferior mirage, where the road ahead appears wet or reflective, as if covered by a pool of water, even though it is dry. Understanding mirages requires knowledge of how light bends when it passes through air layers of different temperatures and densities. This question asks what atmospheric condition leads to the formation of such mirages.
Given Data / Assumptions:
Concept / Approach:
The key idea is that the refractive index of air depends on its density, which in turn depends on temperature. Hot air near the ground is less dense and has a slightly lower refractive index than cooler air above it. When there is a strong temperature gradient, light rays travelling from distant objects bend gradually as they pass through layers of air with different refractive indices. In an inferior mirage, some rays curve upward after approaching the hot layer near the ground and reach the observer eye as if they came from the ground. The brain interprets these rays as reflections, creating the illusion of water or a shiny surface.
Step-by-Step Solution:
Step 1: Recognise that the ground becomes very hot in strong sunlight and heats the air just above it.
Step 2: The air close to the surface becomes hotter and less dense than the cooler air higher up.
Step 3: Because refractive index of air decreases slightly with decreasing density, the hot near surface air has a lower refractive index than the cooler air above.
Step 4: Light rays from distant objects entering this region experience a continuous change in refractive index and bend according to Snell law in a graded medium.
Step 5: Some rays bend upward after approaching the hot layer, so they reach the observer from directions that would normally correspond to reflections from the ground.
Step 6: The observer brain interprets these rays as if they were coming from a shiny or watery surface, producing the mirage of water.
Verification / Alternative check:
Mirages are rarely seen on cool, cloudy days when the ground and air temperatures are more uniform, but they are common on hot sunny days when asphalt or sand is strongly heated. This correlation between strong heating and mirage formation supports the explanation based on unequal heating and resulting density gradients. Physics demonstrations using tanks of liquid with carefully layered refractive indices can reproduce similar bending of light and inverted images, showing that gradients in refractive index are sufficient to create mirage like effects.
Why Other Options Are Wrong:
Magnetic disturbances: Earth magnetic field and ordinary magnetic disturbances do not significantly affect the path of visible light in air and are not responsible for mirages.
Equal heating of different parts of the atmosphere: If the air were heated uniformly, there would be no strong refractive index gradients and no mirage of this type.
Depletion of the ozone layer: Ozone layer changes affect ultraviolet radiation absorption high in the atmosphere but do not directly cause the local refractive effects that produce road level mirages.
Common Pitfalls:
Some learners think the apparent water must be due to actual moisture on the road or to reflections from the sky alone. While the sky reflection contributes to the visual impression, the essential mechanism is the bending of light in layers of air with different refractive indices created by unequal heating. Another confusion is to attribute many atmospheric optical phenomena, such as rainbows or mirages, to a single cause; in reality, rainbows are due to refraction and reflection in water droplets, whereas mirages arise from refractive index gradients in air.
Final Answer:
A mirage on a hot road is mainly caused by unequal heating of different parts of the atmosphere, producing layers of air with different densities and refractive indices.
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