Rayleigh scattering is what makes the dramatic colours of the sunset.

Rayleigh scattering is the main cause of signal loss in optical fibers.

Rayleigh scattering does not change the state of material, hence it is a parametric process.

Rayleigh scattering is the way that light scatters when it hits a very small object.

Rayleigh scattering is an important phenomenon in space.

Form factor program for Rayleigh scattering of gamma rays by bound electrons.

Strongly absorbs red light, so the sky color is a deeper blue than just the Rayleigh scattering would predict.

Rayleigh scattering dominates in such clear air, making the sky appear blue in the daytime.

The appearance of blue, green and hazel eyes result from the Rayleigh scattering of light in the iris.

Rayleigh scattering (Why the sky is blue, sunsets are red, and associated phenomena)

Rayleigh scattering is much greater for blue light than for other colours due to its shorter wavelength.

It can be seen from the above equation that Rayleigh scattering is strongly dependent upon the size of the particle and the wavelengths.

Rayleigh scattering defines the amount of scattering of light rays.

Rayleigh scattering is much less frequent.

On a sunny day Rayleigh scattering gives the sky a blue gradient - dark in the zenith, light near the horizon.

Another possibility for the weak Rayleigh scattering is that the planet has a hydrogen-dominated atmosphere with extensive clouds.

Rayleigh scattering is a spectroscopic scattering phenomenon that accounts for the color of the sky.

The Rayleigh scattering of the HeNe gas is, at this time, negligible.

Rayleigh scattering occurs when light particles scatter in a medium without a change in wavelength.

Rayleigh scattering is the dominant elastic scattering mechanism in the X-ray regime.

Rayleigh scattering can be defined as scattering in small size parameter regime .

Ionospheric scattering and Rayleigh scattering are examples of material scattering.

It is sometimes said, incorrectly, that Rayleigh scattering is relevant to imaging techniques such as two-photon.

Rayleigh scattering is defined by a mathematical formula that requires the light-scattering particles to be far smaller than the wavelength of the light.

If the sky has a hydrogen-dominated atmosphere (as shown in the top image) Rayleigh scattering disperses blue light from the atmosphere of the host.