Rayleigh scattering

E179225

Rayleigh scattering is the physical phenomenon in which light or other electromagnetic radiation is elastically scattered by particles much smaller than its wavelength, explaining effects such as the blue color of the daytime sky.

All labels observed (1)

Label Occurrences
Rayleigh scattering canonical 6

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf light scattering mechanism ⓘ
physical phenomenon ⓘ
affects astronomical observations ⓘ
optical communication through atmosphere ⓘ
remote sensing measurements ⓘ
appliesTo particles much smaller than the wavelength of radiation ⓘ
causes partial polarization of skylight ⓘ
contrastedWith Compton scattering ⓘ
Mie scattering ⓘ
Raman scattering ⓘ
linked to: Raman effect
crossSectionDependsOn particle size to the sixth power for small particles ⓘ
crossSectionProportionalTo 1/λ^4 ⓘ
dependsOn polarizability of scattering particles ⓘ
refractive index fluctuations ⓘ
energyChangeOfPhoton approximately zero ⓘ
explains blue color of the daytime sky ⓘ
bluish appearance of distant mountains ⓘ
color of Earth's atmosphere when viewed from space ⓘ
color of smoke and colloidal suspensions in some cases ⓘ
reddish color of sunrise and sunset ⓘ
firstDescribedBy John William Strutt, 3rd Baron Rayleigh ⓘ
linked to: Lord Rayleigh
intensityProportionalTo 1/λ^4 ⓘ
isElastic true ⓘ
isSubtypeOf coherent scattering ⓘ
elastic scattering ⓘ
lessEffectiveAt longer wavelengths ⓘ
mathematicalDescriptionUses classical electromagnetic theory ⓘ
dipole approximation ⓘ
moreEffectiveAt shorter wavelengths ⓘ
namedAfter Lord Rayleigh ⓘ
occursFor molecules in air such as nitrogen and oxygen ⓘ
occursIn Earth's atmosphere ⓘ
gases ⓘ
liquids ⓘ
planetary atmospheres ⓘ
solids with small inhomogeneities ⓘ
occursWhenParticleSizeIs much smaller than wavelength ⓘ
relatedTo Mie theory ⓘ
Tyndall effect ⓘ
requiresCondition particle diameter much less than wavelength (d << λ) ⓘ
scatters electromagnetic radiation ⓘ
light ⓘ
studiedIn astrophysics ⓘ
atmospheric optics ⓘ
climate science ⓘ
optics ⓘ
usedToCorrect atmospheric effects in satellite imagery ⓘ
wavelengthDependence inversely proportional to the fourth power of wavelength ⓘ
yearCharacterizedApprox 1871 ⓘ

How these facts were elicited

Referenced by (6)

Full triples — surface form annotated when it differs from this entity's canonical label.

Lord Rayleigh → knownFor → Rayleigh scattering ⓘ
Tyndall effect → relatedTo → Rayleigh scattering ⓘ
Mie theory → generalizes → Rayleigh scattering ⓘ
John William Strutt, 3rd Baron Rayleigh → knownFor → Rayleigh scattering ⓘ
subject linked to: Rayleigh family