Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Reflectance
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Mathematical definitions== ===Hemispherical reflectance=== The ''hemispherical reflectance'' of a surface, denoted {{mvar|R}}, is defined as<ref name="ISO_9288-1989">{{cite web| url=http://www.iso.org/iso/home/store/catalogue_tc/catalogue_detail.htm?csnumber=16943|title=Thermal insulation — Heat transfer by radiation — Physical quantities and definitions|work=ISO 9288:1989|publisher=[[International Organization for Standardization|ISO]] catalogue|year=1989|access-date=2015-03-15}}</ref> <math display="block">R = \frac{\Phi_\mathrm{e}^\mathrm{r}}{\Phi_\mathrm{e}^\mathrm{i}},</math> where {{math|Φ<sub>e</sub><sup>r</sup>}} is the [[radiant flux]] ''reflected'' by that surface and {{math|Φ<sub>e</sub><sup>i</sup>}} is the radiant flux ''received'' by that surface. ===Spectral hemispherical reflectance=== The ''spectral hemispherical reflectance in frequency'' and ''spectral hemispherical reflectance in wavelength'' of a surface, denoted {{math|''R''<sub>''ν''</sub>}} and {{math|''R''<sub>''λ''</sub>}} respectively, are defined as<ref name="ISO_9288-1989" /> <math display="block">R_\nu = \frac{\Phi_{\mathrm{e},\nu}^\mathrm{r}}{\Phi_{\mathrm{e},\nu}^\mathrm{i}},</math> <math display="block">R_\lambda = \frac{\Phi_{\mathrm{e},\lambda}^\mathrm{r}}{\Phi_{\mathrm{e},\lambda}^\mathrm{i}},</math> where *{{math|Φ<sub>e,''ν''</sub><sup>r</sup>}} is the [[Radiant flux|spectral radiant flux in frequency]] ''reflected'' by that surface; *{{math|Φ<sub>e,''ν''</sub><sup>i</sup>}} is the spectral radiant flux in frequency received by that surface; *{{math|Φ<sub>e,''λ''</sub><sup>r</sup>}} is the [[Radiant flux|spectral radiant flux in wavelength]] ''reflected'' by that surface; *{{math|Φ<sub>e,''λ''</sub><sup>i</sup>}} is the spectral radiant flux in wavelength received by that surface. ===Directional reflectance=== The ''directional reflectance'' of a surface, denoted ''R''<sub>Ω</sub>, is defined as<ref name="ISO_9288-1989" /> <math display="block">R_\Omega = \frac{L_{\mathrm{e},\Omega}^\mathrm{r}}{L_{\mathrm{e},\Omega}^\mathrm{i}},</math> where *{{math|''L''<sub>e,Ω</sub><sup>r</sup>}} is the [[radiance]] ''reflected'' by that surface; *{{math|''L''<sub>e,Ω</sub><sup>i</sup>}} is the radiance received by that surface. This depends on both the reflected direction and the incoming direction. In other words, it has a value for every combination of incoming and outgoing directions. It is related to the [[bidirectional reflectance distribution function]] and its upper limit is 1. Another measure of reflectance, depending only on the outgoing direction, is ''I''/''F'', where ''I'' is the radiance reflected in a given direction and ''F'' is the incoming radiance averaged over all directions, in other words, the total flux of radiation hitting the surface per unit area, divided by π.<ref>{{cite journal |first1=Jeffrey |last1=Cuzzi |first2=Lindsey |last2=Chambers |first3=Amanda |last3=Hendrix |title=Rough Surfaces: is the dark stuff just shadow? |journal=[[Icarus (journal)|Icarus]] |date=Oct 21, 2016 |volume=289 |pages=281–294 |doi=10.1016/j.icarus.2016.10.018 |pmid=31708591 |pmc=6839776 }}</ref> This can be greater than 1 for a glossy surface illuminated by a source such as the sun, with the reflectance measured in the direction of maximum radiance (see also [[Seeliger effect]]). ===Spectral directional reflectance=== The ''spectral directional reflectance in frequency'' and ''spectral directional reflectance in wavelength'' of a surface, denoted {{math|''R''<sub>Ω,''ν''</sub>}} and {{math|''R''<sub>Ω,''λ''</sub>}} respectively, are defined as<ref name="ISO_9288-1989" /> <math display="block">R_{\Omega,\nu} = \frac{L_{\mathrm{e},\Omega,\nu}^\mathrm{r}}{L_{\mathrm{e},\Omega,\nu}^\mathrm{i}},</math> <math display="block">R_{\Omega,\lambda} = \frac{L_{\mathrm{e},\Omega,\lambda}^\mathrm{r}}{L_{\mathrm{e},\Omega,\lambda}^\mathrm{i}},</math> where *{{math|''L''<sub>e,Ω,''ν''</sub><sup>r</sup>}} is the [[Radiance|spectral radiance in frequency]] ''reflected'' by that surface; *{{math|''L''<sub>e,Ω,''ν''</sub><sup>i</sup>}} is the spectral radiance received by that surface; *{{math|''L''<sub>e,Ω,''λ''</sub><sup>r</sup>}} is the [[Radiance|spectral radiance in wavelength]] ''reflected'' by that surface; *{{math|''L''<sub>e,Ω,''λ''</sub><sup>i</sup>}} is the spectral radiance in wavelength received by that surface. Again, one can also define a value of {{math|''I''/''F''}} (see above) for a given wavelength.<ref>See for example {{cite journal | display-authors=etal |last1=P.G.J Irwin |title=Hazy Blue Worlds: A Holistic Aerosol Model for Uranus and Neptune, Including Dark Spots |journal=Journal of Geophysical Research: Planets | date=Jan 12, 2022 |volume=127 |issue=6 |pages=e2022JE007189 |doi=10.1029/2022JE007189 |pmid=35865671 |pmc=9286428 |arxiv=2201.04516 |bibcode=2022JGRE..12707189I |hdl=1983/65ee78f0-1d28-4017-bbd9-1b49b24700d7 |s2cid=245877540 |bibcode-access=free |doi-access=free |hdl-access=free |s2cid-access=free }}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)