Comparison of photometric and radiometric quantities

Radiometry is a set of techniques for measuring electromagnetic radiation, including visible light. Radiometric techniques in optics characterize the distribution of the radiation's power in space, as opposed to photometric techniques, which characterize the light's interaction with the human eye.

The fundamental difference between radiometry and photometry is that radiometry can cover the entire optical radiation spectrum, while photometry is limited to the visible spectrum. However, some definitions of radiometry include other portions of the electromagnetic radiation spectrum, and some glossaries define photometry such that associated quantities are weighted by wavelength according to the spectral sensitivity of the human visual system. Photometry can therefore be considered a kind of radiometry. Radiometry is distinct from quantum techniques such as photon counting.

The use of radiometers to determine the temperature of objects and gasses by measuring radiation flux is called pyrometry. Handheld pyrometer devices are often marketed as infrared thermometers.

Radiometry is important in astronomy, especially radio astronomy, and plays a significant role in Earth remote sensing. The measurement techniques categorized as radiometry in optics are called photometry in some astronomical applications, contrary to the optics usage of the term.

Spectroradiometry is the measurement of absolute radiometric quantities in narrow bands of wavelength.

Radiometric quantities

SI radiometry unitsvte
QuantityUnitDimensionNotes
NameSymbolNameSymbol
Radiant energyQejouleJML2⋅T−2Energy of electromagnetic radiation.
Radiant energy densitywejoule per cubic metreJ/m3ML−1⋅T−2Radiant energy per unit volume.
Radiant fluxΦewattW = J/sML2⋅T−3Radiant energy emitted, reflected, transmitted or received, per unit time. This is sometimes also called "radiant power", and called luminosity in astronomy.
Spectral fluxΦe,νwatt per hertzW/HzML2⋅T−2Radiant flux per unit frequency or wavelength. The latter is commonly measured in W⋅nm−1.
Φe,λwatt per metreW/mMLT−3
Radiant intensityIe,Ωwatt per steradianW/srML2⋅T−3Radiant flux emitted, reflected, transmitted or received, per unit solid angle. This is a directional quantity.
Spectral intensityIe,Ω,νwatt per steradian per hertzW⋅sr−1⋅Hz−1ML2⋅T−2Radiant intensity per unit frequency or wavelength. The latter is commonly measured in W⋅sr−1⋅nm−1. This is a directional quantity.
Ie,Ω,λwatt per steradian per metreW⋅sr−1⋅m−1MLT−3
RadianceLe,Ωwatt per steradian per square metreW⋅sr−1⋅m−2MT−3Radiant flux emitted, reflected, transmitted or received by a surface, per unit solid angle per unit projected area. This is a directional quantity. This is sometimes also called "intensity".
Spectral radiance Specific intensityLe,Ω,νwatt per steradian per square metre per hertzW⋅sr−1⋅m−2⋅Hz−1MT−2Radiance of a surface per unit frequency or wavelength. The latter is commonly measured in W⋅sr−1⋅m−2⋅nm−1. This is a directional quantity. This is sometimes also called "spectral intensity".
Le,Ω,λwatt per steradian per square metre, per metreW⋅sr−1⋅m−3ML−1⋅T−3
Irradiance Flux densityEewatt per square metreW/m2MT−3Radiant flux received by a surface per unit area. This is sometimes also called "intensity".
Spectral irradiance Spectral flux densityEe,νwatt per square metre per hertzW⋅m−2⋅Hz−1MT−2Irradiance of a surface per unit frequency or wavelength. This is sometimes also called "spectral intensity". Non-SI units of spectral flux density include jansky (1 Jy = 10−26 W⋅m−2⋅Hz−1) and solar flux unit (1 sfu = 10−22 W⋅m−2⋅Hz−1 = 104 Jy).
Ee,λwatt per square metre, per metreW/m3ML−1⋅T−3
RadiosityJewatt per square metreW/m2MT−3Radiant flux leaving (emitted, reflected and transmitted by) a surface per unit area. This is sometimes also called "intensity".
Spectral radiosityJe,νwatt per square metre per hertzW⋅m−2⋅Hz−1MT−2Radiosity of a surface per unit frequency or wavelength. The latter is commonly measured in W⋅m−2⋅nm−1. This is sometimes also called "spectral intensity".
Je,λwatt per square metre, per metreW/m3ML−1⋅T−3
Radiant exitanceMewatt per square metreW/m2MT−3Radiant flux emitted by a surface per unit area. This is the emitted component of radiosity. "Radiant emittance" is an old term for this quantity. This is sometimes also called "intensity".
Spectral exitanceMe,νwatt per square metre per hertzW⋅m−2⋅Hz−1MT−2Radiant exitance of a surface per unit frequency or wavelength. The latter is commonly measured in W⋅m−2⋅nm−1. "Spectral emittance" is an old term for this quantity. This is sometimes also called "spectral intensity".
Me,λwatt per square metre, per metreW/m3ML−1⋅T−3
Radiant exposureHejoule per square metreJ/m2MT−2Radiant energy received by a surface per unit area, or equivalently irradiance of a surface integrated over time of irradiation. This is sometimes also called "radiant fluence".
Spectral exposureHe,νjoule per square metre per hertzJ⋅m−2⋅Hz−1MT−1Radiant exposure of a surface per unit frequency or wavelength. The latter is commonly measured in J⋅m−2⋅nm−1. This is sometimes also called "spectral fluence".
He,λjoule per square metre, per metreJ/m3ML−1⋅T−2
See also: SIRadiometryPhotometry
Radiometry coefficientsvte
QuantitySI unitsNotes
NameSym.
Hemispherical emissivityε—N/aRadiant exitance of a surface, divided by that of a black body at the same temperature as that surface.
Spectral hemispherical emissivityεν ελ—N/aSpectral exitance of a surface, divided by that of a black body at the same temperature as that surface.
Directional emissivityεΩ—N/aRadiance emitted by a surface, divided by that emitted by a black body at the same temperature as that surface.
Spectral directional emissivityεΩ,ν εΩ,λ—N/aSpectral radiance emitted by a surface, divided by that of a black body at the same temperature as that surface.
Hemispherical absorptanceA—N/aRadiant flux absorbed by a surface, divided by that received by that surface. This should not be confused with "absorbance".
Spectral hemispherical absorptanceAν Aλ—N/aSpectral flux absorbed by a surface, divided by that received by that surface. This should not be confused with "spectral absorbance".
Directional absorptanceAΩ—N/aRadiance absorbed by a surface, divided by the radiance incident onto that surface. This should not be confused with "absorbance".
Spectral directional absorptanceAΩ,ν AΩ,λ—N/aSpectral radiance absorbed by a surface, divided by the spectral radiance incident onto that surface. This should not be confused with "spectral absorbance".
Hemispherical reflectanceR—N/aRadiant flux reflected by a surface, divided by that received by that surface.
Spectral hemispherical reflectanceRν Rλ—N/aSpectral flux reflected by a surface, divided by that received by that surface.
Directional reflectanceRΩ—N/aRadiance reflected by a surface, divided by that received by that surface.
Spectral directional reflectanceRΩ,ν RΩ,λ—N/aSpectral radiance reflected by a surface, divided by that received by that surface.
Hemispherical transmittanceT—N/aRadiant flux transmitted by a surface, divided by that received by that surface.
Spectral hemispherical transmittanceTν Tλ—N/aSpectral flux transmitted by a surface, divided by that received by that surface.
Directional transmittanceTΩ—N/aRadiance transmitted by a surface, divided by that received by that surface.
Spectral directional transmittanceTΩ,ν TΩ,λ—N/aSpectral radiance transmitted by a surface, divided by that received by that surface.
Hemispherical attenuation coefficientμm−1Radiant flux absorbed and scattered by a volume per unit length, divided by that received by that volume.
Spectral hemispherical attenuation coefficientμν μλm−1Spectral radiant flux absorbed and scattered by a volume per unit length, divided by that received by that volume.
Directional attenuation coefficientμΩm−1Radiance absorbed and scattered by a volume per unit length, divided by that received by that volume.
Spectral directional attenuation coefficientμΩ,ν μΩ,λm−1Spectral radiance absorbed and scattered by a volume per unit length, divided by that received by that volume.

Integral and spectral radiometric quantities

Integral quantities (like radiant flux) describe the total effect of radiation of all wavelengths or frequencies, while spectral quantities (like spectral power) describe the effect of radiation of a single wavelength λ or frequency ν. To each integral quantity there are corresponding spectral quantities, defined as the quotient of the integrated quantity by the range of frequency or wavelength considered. For example, the radiant flux Φe corresponds to the spectral power Φe,λ and Φe,ν.

Getting an integral quantity's spectral counterpart requires a limit transition. This comes from the idea that the precisely requested wavelength photon existence probability is zero. Let us show the relation between them using the radiant flux as an example:

Integral flux, whose unit is W: Φ e . {\displaystyle \Phi _{\mathrm {e} }.} Spectral flux by wavelength, whose unit is W/m: Φ e , λ = d Φ e d λ , {\displaystyle \Phi _{\mathrm {e} ,\lambda }={d\Phi _{\mathrm {e} } \over d\lambda },} where d Φ e {\displaystyle d\Phi _{\mathrm {e} }} is the radiant flux of the radiation in a small wavelength interval [ λ − d λ 2 , λ + d λ 2 ] {\displaystyle [\lambda -{d\lambda \over 2},\lambda +{d\lambda \over 2}]}. The area under a plot with wavelength horizontal axis equals to the total radiant flux.

Spectral flux by frequency, whose unit is W/Hz: Φ e , ν = d Φ e d ν , {\displaystyle \Phi _{\mathrm {e} ,\nu }={d\Phi _{\mathrm {e} } \over d\nu },} where d Φ e {\displaystyle d\Phi _{\mathrm {e} }} is the radiant flux of the radiation in a small frequency interval [ ν − d ν 2 , ν + d ν 2 ] {\displaystyle [\nu -{d\nu \over 2},\nu +{d\nu \over 2}]}. The area under a plot with frequency horizontal axis equals to the total radiant flux.

The spectral quantities by wavelength λ and frequency ν are related to each other, since the product of the two variables is the speed of light (λ ⋅ ν = c {\displaystyle \lambda \cdot \nu =c}):

Φ e , λ = c λ 2 Φ e , ν , {\displaystyle \Phi _{\mathrm {e} ,\lambda }={c \over \lambda ^{2}}\Phi _{\mathrm {e} ,\nu },} or Φ e , ν = c ν 2 Φ e , λ , {\displaystyle \Phi _{\mathrm {e} ,\nu }={c \over \nu ^{2}}\Phi _{\mathrm {e} ,\lambda },} or λ Φ e , λ = ν Φ e , ν . {\displaystyle \lambda \Phi _{\mathrm {e} ,\lambda }=\nu \Phi _{\mathrm {e} ,\nu }.}

The integral quantity can be obtained by the spectral quantity's integration:

Φ e = ∫ 0 ∞ Φ e , λ d λ = ∫ 0 ∞ Φ e , ν d ν = ∫ 0 ∞ λ Φ e , λ d ln ⁡ λ = ∫ 0 ∞ ν Φ e , ν d ln ⁡ ν . {\displaystyle \Phi _{\mathrm {e} }=\int _{0}^{\infty }\Phi _{\mathrm {e} ,\lambda }\,d\lambda =\int _{0}^{\infty }\Phi _{\mathrm {e} ,\nu }\,d\nu =\int _{0}^{\infty }\lambda \Phi _{\mathrm {e} ,\lambda }\,d\ln \lambda =\int _{0}^{\infty }\nu \Phi _{\mathrm {e} ,\nu }\,d\ln \nu .}

See also

External links

  • Professor Jim Palmer's Radiometry FAQ page (The University of Arizona College of Optical Sciences).