What is the difference between Rayleigh Tindall and Mie scattering?

Rayleigh scattering involves molecular scatterers that are MUCH smaller than the wavelength of the incident light. Mie scattering involves particles that are much larger than a single molecule. The objects that produce Mie scattering are roughly the same size as the wavelengths of the scattering radiation.

How does Mie scattering occur?

Mie scattering occurs when the diameters of atmospheric particulates are similar to or larger than the wavelengths of the scattered light. Dust, pollen, smoke and microscopic water droplets that form clouds are common causes of Mie scattering.

Is Mie scattering more wavelength selective than Rayleigh scattering?

The scattered light is almost at the same wavelength as the incident light, i. e. Rayleigh scattering is not species selective. Rayleigh scattering is much weaker than Mie scattering but more than two orders of magnitude stronger than Spontaneous Raman Scattering.

How is Rayleigh scattering similar to and different from Mie scattering?

The scattering from molecules and very tiny particles (< 1 /10 wavelength) is predominantly Rayleigh scattering. For particle sizes larger than a wavelength, Mie scattering predominates. This scattering produces a pattern like an antenna lobe, with a sharper and more intense forward lobe for larger particles.

What is Rayleigh scattering in optical fiber?

Rayleigh scattering is a common scattering optical phenomenon, named after the British physicist Lord Rayleigh. It is linear scattering of light at scattering centers which are much smaller than the wavelength of the light. Scattering centers for Rayleigh scattering can be individual atoms or molecules.

What is a Mie resonator?

Abstract. Mie resonator arrays formed by embossing titanium dioxide (TiO2) nanoparticles (NPs) from solution are investigated as optical coatings for anti-reflection applications. Compacted nanoparticle assemblies offer unique possibilities to tailor the effective refractive index (RI).

What causes Rayleigh scattering?

The blue color of the sky is caused by the scattering of sunlight off the molecules of the atmosphere. This scattering, called Rayleigh scattering, is more effective at short wavelengths (the blue end of the visible spectrum).

What visible effects does Rayleigh scattering cause?

Rayleigh scattering of sunlight in Earth’s atmosphere causes diffuse sky radiation, which is the reason for the blue color of the daytime and twilight sky, as well as the yellowish to reddish hue of the low Sun.