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Radiative flux

From Wikipedia, the free encyclopedia
Amount of power radiated through a given area

Radiative flux, also known asradiative flux density orradiation flux (or sometimespower flux density[1]), is the amount ofpower radiated through a given area, in the form ofphotons or other elementary particles, typically expressed in watts per square meter (W/m2).[2] It is used inastronomy to determine themagnitude andspectral class of a star and inmeteorology to determine the intensity of the convection in theplanetary boundary layer. Radiative flux also acts as a generalization ofheat flux, which is equal to the radiative flux when restricted to theinfrared spectrum.

When radiative flux is incident on a surface, it is often calledirradiance. Flux emitted from a surface may be calledradiant exitance orradiant emittance. The ratio of irradiance reflected to the irradiance received by a surface is calledalbedo.

Geophysics

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Shortwave

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In geophysics,shortwave flux is a result of specular and diffuse reflection of incident shortwave radiation by the underlying surface.[3] This shortwave radiation, as solar radiation, can have a profound impact on certain biophysical processes of vegetation, such as canopy photosynthesis and land surface energy budgets, by being absorbed into the soil and canopies.[4] As it is the main energy source of most weather phenomena, the solar shortwave radiation is used extensively innumerical weather prediction.

Longwave

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Longwave flux is a product of bothdownwelling infrared energy as well as emission by the underlying surface. The cooling associated with the divergence of longwave radiation is necessary for creating and sustaining lastinginversion layers close to the surface during polar night. Longwave radiation flux divergence also plays a role in the formation of fog.[5]

SI radiometry units

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SI radiometry units
QuantityUnitDimensionNotes
NameSymbol[nb 1]NameSymbol
Radiant energyQe[nb 2]jouleJML2T−2Energy of electromagnetic radiation.
Radiant energy densitywejoule per cubic metreJ/m3ML−1T−2Radiant energy per unit volume.
Radiant fluxΦe[nb 2]wattW = J/sML2T−3Radiant energy emitted, reflected, transmitted or received, per unit time. This is sometimes also called "radiant power", and calledluminosity in astronomy.
Spectral fluxΦe,ν[nb 3]watt perhertzW/HzML2T −2Radiant flux per unit frequency or wavelength. The latter is commonly measured in W⋅nm−1.
Φe,λ[nb 4]watt per metreW/mMLT−3
Radiant intensityIe,Ω[nb 5]watt persteradianW/srML2T−3Radiant flux emitted, reflected, transmitted or received, per unit solid angle. This is adirectional quantity.
Spectral intensityIe,Ω,ν[nb 3]watt per steradian per hertzW⋅sr−1⋅Hz−1ML2T−2Radiant intensity per unit frequency or wavelength. The latter is commonly measured in W⋅sr−1⋅nm−1. This is adirectional quantity.
Ie,Ω,λ[nb 4]watt per steradian per metreW⋅sr−1⋅m−1MLT−3
RadianceLe,Ω[nb 5]watt per steradian per square metreW⋅sr−1⋅m−2MT−3Radiant flux emitted, reflected, transmitted or received by asurface, per unit solid angle per unit projected area. This is adirectional quantity. This is sometimes also confusingly called "intensity".
Spectral radiance
Specific intensity
Le,Ω,ν[nb 3]watt per steradian per square metre per hertzW⋅sr−1⋅m−2⋅Hz−1MT−2Radiance of asurface per unit frequency or wavelength. The latter is commonly measured in W⋅sr−1⋅m−2⋅nm−1. This is adirectional quantity. This is sometimes also confusingly called "spectral intensity".
Le,Ω,λ[nb 4]watt per steradian per square metre, per metreW⋅sr−1⋅m−3ML−1T−3
Irradiance
Flux density
Ee[nb 2]watt per square metreW/m2MT−3Radiant fluxreceived by asurface per unit area. This is sometimes also confusingly called "intensity".
Spectral irradiance
Spectral flux density
Ee,ν[nb 3]watt per square metre per hertzW⋅m−2⋅Hz−1MT−2Irradiance of asurface per unit frequency or wavelength. This is sometimes also confusingly called "spectral intensity". Non-SI units of spectral flux density includejansky (1 Jy =10−26 W⋅m−2⋅Hz−1) andsolar flux unit (1 sfu =10−22 W⋅m−2⋅Hz−1 =104 Jy).
Ee,λ[nb 4]watt per square metre, per metreW/m3ML−1T−3
RadiosityJe[nb 2]watt per square metreW/m2MT−3Radiant fluxleaving (emitted, reflected and transmitted by) asurface per unit area. This is sometimes also confusingly called "intensity".
Spectral radiosityJe,ν[nb 3]watt per square metre per hertzW⋅m−2⋅Hz−1MT−2Radiosity of asurface per unit frequency or wavelength. The latter is commonly measured in W⋅m−2⋅nm−1. This is sometimes also confusingly called "spectral intensity".
Je,λ[nb 4]watt per square metre, per metreW/m3ML−1T−3
Radiant exitanceMe[nb 2]watt per square metreW/m2MT−3Radiant fluxemitted by asurface per unit area. This is the emitted component of radiosity. "Radiant emittance" is an old term for this quantity. This is sometimes also confusingly called "intensity".
Spectral exitanceMe,ν[nb 3]watt per square metre per hertzW⋅m−2⋅Hz−1MT−2Radiant exitance of asurface 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 confusingly called "spectral intensity".
Me,λ[nb 4]watt per square metre, per metreW/m3ML−1T−3
Radiant exposureHejoule per square metreJ/m2MT−2Radiant energy received by asurface per unit area, or equivalently irradiance of asurface integrated over time of irradiation. This is sometimes also called "radiant fluence".
Spectral exposureHe,ν[nb 3]joule per square metre per hertzJ⋅m−2⋅Hz−1MT−1Radiant exposure of asurface per unit frequency or wavelength. The latter is commonly measured in J⋅m−2⋅nm−1. This is sometimes also called "spectral fluence".
He,λ[nb 4]joule per square metre, per metreJ/m3ML−1T−2
See also:
  1. ^Standards organizations recommend that radiometricquantities should be denoted with suffix "e" (for "energetic") to avoid confusion with photometric orphoton quantities.
  2. ^abcdeAlternative symbols sometimes seen:W orE for radiant energy,P orF for radiant flux,I for irradiance,W for radiant exitance.
  3. ^abcdefgSpectral quantities given per unitfrequency are denoted with suffix "ν" (Greek letternu, not to be confused with a letter "v", indicating a photometric quantity.)
  4. ^abcdefgSpectral quantities given per unitwavelength are denoted with suffix "λ".
  5. ^abDirectional quantities are denoted with suffix "Ω".

See also

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References

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  1. ^"Communication Systems/Wireless Transmission".WikiBooks: Communication Systems/Wireless Transmission. Retrieved2018-12-11.
  2. ^"Glossary of Meteorology: Radiative Flux". Retrieved2008-12-24.
  3. ^Kantha, L.H.;Clayson, Carol (2000).Small scale processes in geophysical fluid flow. San Diego: Academic Press.
  4. ^Yang, Rongqian; Friedl, Mark A.; Ni, Wenge (July 16, 2001)."Parameterization of shortwave radiation fluxes for nonuniform vegetation canopies in land surface models".Journal of Geophysical Research.106 (D13):14275–14286.Bibcode:2001JGR...10614275Y.doi:10.1029/2001JD900180.
  5. ^Hoch, S. W.; Calanca, P.; Philipona, R.; Ohmura, A. (2007)."Year-Round Observation of Longwave Radiative Flux Divergence in Greenland".Journal of Applied Meteorology and Climatology.46 (9):1469–1479.Bibcode:2007JApMC..46.1469H.doi:10.1175/JAM2542.1.
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