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
Solar constant
(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!
==Calculation== [[Solar irradiance]] is measured by satellites above [[Earth's atmosphere]],<ref name=TSI20>{{cite web|url=http://acrim.com/TSI%20Monitoring.htm|title=Satellite observations of total solar irradiance|website=acrim.com|access-date=2010-10-02|archive-date=2011-07-16|archive-url=https://web.archive.org/web/20110716140550/http://www.acrim.com/TSI%20Monitoring.htm|url-status=dead}}</ref> and is then adjusted using the [[inverse square law]] to infer the magnitude of solar irradiance at one [[Astronomical Unit]] (au) to evaluate the solar constant.<ref>{{Cite web | url=http://www.ngdc.noaa.gov/stp/SOLAR/ftpsolarirradiance.html | archive-url=https://archive.today/20031204001103/http://www.ngdc.noaa.gov/stp/SOLAR/ftpsolarirradiance.html | url-status=dead | archive-date=December 4, 2003 | title=NOAA Status Alert}}</ref> The approximate average value cited,<ref name=KoppLean11/> 1.3608 Β± 0.0005 kW/m<sup>2</sup>, which is 81.65 kJ/m<sup>2</sup> per minute, is equivalent to approximately 1.951 calories per minute per square centimeter, or 1.951 [[Langley (unit)|langleys]] per minute. Solar output is nearly, but not quite, constant. Variations in [[total solar irradiance]] (TSI) were small and difficult to detect accurately with technology available before the satellite era (Β±2% in 1954). Total solar output is now measured as varying (over the last three 11-year [[sunspot]] cycles) by approximately 0.1%;<ref name=Willson91>{{cite journal |last=Willson |first=Richard C.|author2=H.S. Hudson|date=1991 |title=The Sun's luminosity over a complete solar cycle |journal=Nature |volume=351 |issue=6321 |pages=42β4 |doi=10.1038/351042a0 |bibcode=1991Natur.351...42W|s2cid=4273483}}<!-- {{harvnb|Willson|1991}} --></ref> see [[solar variation]] for details. ===For extrasolar planets=== <math>L=4\pi R_{\rm star}^2\sigma T_{\rm star}^4</math> <br> <math>L=4\pi f \ d ^2</math> <br> Therefore: <math>4\pi f\ d ^2 = 4\pi R_{\rm star}^2\sigma T_{\rm star}^4</math> <br> <math display="block"> f= \left ( \frac{R_{\rm star}^2\sigma T_{\rm star}^4}{ d ^2} \right ) </math> <br> Where <math>\sigma</math> is the Stefan-Boltzmann constant (<math>\approx 5.67e^{-8} W m^{-2} K^{-4}</math>) and f is the irradiance of the star at the extrasolar planet at distance d.
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)