To determine the wavelength or colour at which solar radiation peaks, we need to consider the solar spectrum and the concept of blackbody radiation. The Sun emits radiation across various wavelengths, but the intensity of this radiation is not uniform across the spectrum.
According to Wien's Displacement Law, the wavelength at which the emission of a blackbody spectrum is at its maximum is inversely proportional to its temperature. The formula for Wien's Law is:
\(\lambda_{\text{max}} = \frac{b}{T}\)
where:
Calculating the peak wavelength for the Sun:
\(\lambda_{\text{max}} = \frac{2.897 \times 10^{-3} \, \text{m K}}{5778 \, \text{K}} \approx 500 \, \text{nm}\)
The peak wavelength of approximately 500 nm falls within the visible spectrum, specifically in the green region. This means that the Sun's radiation peaks at green light.
Conclusion: The wavelength/colour at which solar radiation peaks is green, hence the correct answer is green.
By understanding the solar radiation and its peak emission, we can conclude that during the daytime, the sunlight appears white because it is a mixture of all colors, even though it peaks in the green wavelength.
| A. | Rainbows | P. | Refraction |
| B. | Mirage | Q. | Refraction and Reflection |
| C. | Corona | R. | Refraction, Reflection, Dispersion in ice crystals |
| D. | Halo | S. | Diffraction |

Air rises from point A to C. At point C it reaches the dew point and begins to descend on the leeward side because it is colder than its surroundings. What will happen to the temperature of the descending air?
Read the following statements about land and sea breeze and choose the CORRECT answer.
I. The land breeze is less extensive both vertically and horizontally than the sea breeze
II. Temperature differences between land and sea are rarely as great at night as in the day time.