Wien's distribution law
From Glossary of Meteorology
A relation, derived on purely thermodynamic reasoning by Wien, between the monochromatic emittance of an ideal blackbody and that body's temperature.
Compare Wien's law.
where eλ is the monochromatic emittance (emissive power) of a blackbody at wavelength λ and absolute temperature T, and f(λT) a function that cannot be determined purely on classical thermodynamic grounds. The specification of f(λT) by Planck in 1901 formed the beginning of modern quantum theory.
Compare Wien's law.