Problem 14
Question
The blue colour of the sky is due to (a) scattering of light from particles of dust in the atmosphere (b) scattering of light from the sun (c) scattering of light due to the ozone layer (d) all of these
Step-by-Step Solution
Verified Answer
The blue color of the sky is mainly due to Rayleigh scattering by air molecules, not dust. Option (b) would be closest if it specified that.
1Step 1: Understanding the Phenomenon
The blue color of the sky is primarily due to the scattering of light by particles in the Earth's atmosphere. This phenomenon is called 'Rayleigh scattering'. It occurs when the molecules in the air scatter the shorter wavelengths of light (blue and violet) more than the longer wavelengths (red). However, our eyes are more sensitive to blue light, and the presence of some filtering effects in the atmosphere means we see a blue sky.
2Step 2: Examining the Options
Let's go through the options: Option (a) suggests scattering by dust particles, which is not the primary reason for the sky's blue color, as Rayleigh scattering is due to air molecules, not dust particles. Option (b) mentions scattering of light from the sun; this is partially correct but vague, as it doesn't specify the mechanism (Rayleigh scattering by molecules). Option (c) mentions the ozone layer, which does absorb and scatter light but is not responsible for the blue sky. Option (d) states 'all of these', which is incorrect because not all the options accurately contribute to the blue color as explained.
3Step 3: Choosing the Correct Answer
Given the understanding that Rayleigh scattering from molecules in the atmosphere primarily causes the blue color of the sky, the correct answer aligns with scattering due to this specific cause. Options (b) and (c) are incorrect as they don't accurately describe the cause. Therefore, none of the options accurately describe the entire phenomenon completely, but option (b) is the closest if it referred specifically to Rayleigh scattering.
Key Concepts
Atmospheric ScatteringLight WavelengthsBlue Sky Phenomenon
Atmospheric Scattering
Atmospheric scattering is a crucial phenomenon that helps us understand many atmospheric optical phenomena, including why the sky appears blue.
When sunlight enters our atmosphere, it does not travel in straight lines. Instead, it interacts with the molecules of gases such as nitrogen and oxygen, resulting in scattering.
The key mechanism at play here is known as Rayleigh scattering. This phenomenon is more effective at scattering shorter wavelengths of light (like blue and violet) compared to longer wavelengths (like red).
Since the air molecules are smaller than the wavelength of visible light, Rayleigh scattering prefers these shorter wavelengths. However, the abundance of blue light and its greater sensitivity to our eyes make the sky appear predominantly blue. It's fascinating to realize that without this scattering effect, the sky would look vastly different.
When sunlight enters our atmosphere, it does not travel in straight lines. Instead, it interacts with the molecules of gases such as nitrogen and oxygen, resulting in scattering.
The key mechanism at play here is known as Rayleigh scattering. This phenomenon is more effective at scattering shorter wavelengths of light (like blue and violet) compared to longer wavelengths (like red).
Since the air molecules are smaller than the wavelength of visible light, Rayleigh scattering prefers these shorter wavelengths. However, the abundance of blue light and its greater sensitivity to our eyes make the sky appear predominantly blue. It's fascinating to realize that without this scattering effect, the sky would look vastly different.
Light Wavelengths
Light is a form of electromagnetic radiation and is composed of various colors each defined by their specific wavelength. These colors range from violet, which has the shortest wavelength, to red, which has the longest.
When light interacts with the Earth's atmosphere, the behavior of its components changes. Blue and violet colors possess shorter wavelengths and are scattered more efficiently by atmospheric particles.
When light interacts with the Earth's atmosphere, the behavior of its components changes. Blue and violet colors possess shorter wavelengths and are scattered more efficiently by atmospheric particles.
- Violet light is scattered even more than blue, but it doesn't dominate the sky's color because the human eye is less sensitive to it.
- In addition, some of the violet light is absorbed by the upper atmosphere, reducing its visibility.
Blue Sky Phenomenon
The beautiful blue sky we see during the day is largely due to the Rayleigh scattering of sunlight by atmospheric molecules.
While sunlight consists of all colors in the spectrum, the shorter blue wavelengths are scattered in many more directions than the other colors when they strike tiny molecules in our atmosphere.
Yet, you might wonder why the sky doesn't seem to include the violet part of the spectrum if it's also heavily scattered. This is because:
While sunlight consists of all colors in the spectrum, the shorter blue wavelengths are scattered in many more directions than the other colors when they strike tiny molecules in our atmosphere.
Yet, you might wonder why the sky doesn't seem to include the violet part of the spectrum if it's also heavily scattered. This is because:
- The sensitivity of the human eye is greater for blue light than for violet light, which means we predominantly perceive the sky as blue rather than purple.
- Additional absorption and scattering processes further tend to favor the blue end of the spectrum.
Other exercises in this chapter
Problem 12
The volume of gases \(\mathrm{H}_{2}, \mathrm{CH}_{4}, \mathrm{CO}_{2}\) and \(\mathrm{NH}_{3}\) absorbed by \(1 \mathrm{~g}\) of charcoal at \(288 \mathrm{~K}\
View solution Problem 13
Hardy-Schulze law states that (a) Larger the size of the coagulating ions, greater is the coagulating power, having opposite sign of solution (b) Solution must
View solution Problem 15
The coagulating power of an effective ion carrying the charge opposite to the sol particles is given by (a) Brownian movement (b) Gold number (c) Tyndall effect
View solution Problem 16
On adding few drops of dilute HCl to freshly precipitated ferric hydroxide, a red coloured colloidal solution is obtained. This phenomenon is known as (a) Pepti
View solution