SUMMARY
The sky appears white on the horizon due to a combination of scattering phenomena, primarily Rayleigh Scattering, Mie Scattering, and Nonspecific Scattering. These scattering types occur based on the size of atmospheric particles relative to light wavelengths. In humid conditions, larger particles lead to more Nonspecific Scattering, resulting in a white hue. Additionally, the presence of dust and pollution contributes to the lighter appearance of the sky near the horizon, while clear, dry air enhances the deep blue color of the sky.
PREREQUISITES
- Understanding of Rayleigh Scattering, Mie Scattering, and Nonspecific Scattering
- Knowledge of atmospheric composition and its effects on light
- Familiarity with the relationship between humidity and light scattering
- Basic principles of light wavelength and particle size interactions
NEXT STEPS
- Research the effects of humidity on light scattering in the atmosphere
- Study the differences between Rayleigh and Mie Scattering in detail
- Explore the impact of air pollution on sky color and visibility
- Investigate the role of temperature in atmospheric conditions and sky coloration
USEFUL FOR
Atmospheric scientists, meteorologists, educators in environmental science, and anyone interested in the optical phenomena of the sky.