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
Earth radius
(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!
{{for multi|its historical development|Spherical Earth|its determination|Arc measurement}} {{short description|Distance from the Earth surface to a point near its center}} {{Infobox quantity | name = Earth radius | othernames = terrestrial radius | width = | background = | image = WGS84_mean_Earth_radius.svg | caption = Equatorial (''a''), polar (''b'') and arithmetic mean Earth radii as defined in the 1984 [[World Geodetic System]] revision (not to scale) | unit = meters | otherunits = | symbols = ''R''<sub>π¨</sub>, ''R''<sub>E</sub>, ''a'', ''b'', ''a''<sub>E</sub>, ''b''<sub>E</sub>, ''R''<sub>''e''E</sub>, ''R''<sub>''p''E</sub> | baseunits = [[Metre|m]] | dimension = <math>\mathsf{L}</math> | extensive = | intensive = | conserved = | transformsas = scalar | derivations = | value = ''Equatorial radius'': {{mvar|a}} = ({{val|6378137.0|u=m}}) <br/> ''Polar radius'': {{mvar|b}} = ({{val|6356752.3|u=m}}) }} {{Infobox unit | name = Nominal Earth radius | image = EarthPieSlice.png | caption = Cross section of Earth's Interior | standard = [[astronomy]], [[geophysics]] | quantity = [[distance]] | symbol = <math>\mathcal{R}^\mathrm N_\mathrm{E}</math> | symbol2 = <math>\mathcal{R}^\mathrm N_{e\mathrm{E}}</math>, <math>\mathcal{R}^\mathrm N_{p\mathrm{E}}</math> | units1 = [[SI base unit]] | inunits1 = {{val|6.3781|e=6|u=m}}<ref name = "IAU XXIX">{{cite arXiv |eprint=1510.07674|last1=Mamajek|first1=E. E|title=IAU 2015 Resolution B3 on Recommended Nominal Conversion Constants for Selected Solar and Planetary Properties| last2=Prsa|first2=A|last3=Torres|first3=G|last4=Harmanec|first4=P|last5=Asplund|first5=M|last6=Bennett|first6=P. D|last7=Capitaine|first7=N|last8=Christensen-Dalsgaard|first8=J|last9=Depagne|first9=E|last10=Folkner|first10=W. M|last11=Haberreiter|first11=M|last12=Hekker|first12=S|last13=Hilton|first13=J. L|last14=Kostov|first14=V|last15=Kurtz|first15=D. W|last16=Laskar|first16=J|last17=Mason|first17=B. D|last18=Milone|first18=E. F|last19=Montgomery|first19=M. M|last20=Richards|first20=M. T|last21=Schou|first21=J|last22=Stewart|first22=S. G|class=astro-ph.SR|year=2015|display-authors= 3}}</ref> | units2 = [[Metric system]] | inunits2 = {{val|6357|to|6378|u=km|fmt=commas}} | units3 = [[English units]] | inunits3 = {{val|3950|to|3963|u=mi|fmt=commas}} }} {{Geodesy}} '''Earth radius''' (denoted as ''R''<sub>π¨</sub> or ''R''<sub>E</sub>) is the distance from the center of [[Earth]] to a point on or near its surface. Approximating the [[figure of Earth]] by an [[Earth spheroid]] (an [[oblate ellipsoid]]), the radius ranges from a maximum ('''equatorial radius''', denoted ''a'') of about {{cvt|6378|km|mi}} to a minimum ('''polar radius''', denoted ''b'') of nearly {{cvt|6357|km|mi}}. A globally-average value is usually considered to be {{convert|6371|km|mi}} with a 0.3% variability (Β±10 km) for the following reasons. The [[International Union of Geodesy and Geophysics]] (IUGG) provides three reference values: the ''mean radius'' (''R''{{sub|1}}) of three radii measured at two equator points and a pole; the ''authalic radius'', which is the radius of a sphere with the same surface area (''R''{{sub|2}}); and the ''volumetric radius'', which is the radius of a sphere having the same volume as the ellipsoid (''R''{{sub|3}}).<ref name="Moritz" /> All three values are about {{convert|6371|km|mi}}. Other ways to define and measure the Earth's radius involve either the spheroid's [[radius of curvature]] or the actual [[topography]]. A few definitions yield values outside the range between the [[geographical pole|polar]] radius and [[equator]]ial radius because they account for localized effects. A ''nominal Earth radius'' (denoted <math>\mathcal{R}^\mathrm N_\mathrm{E}</math>) is sometimes used as a [[unit of measurement]] in [[astronomy]] and [[geophysics]], a [[conversion factor]] used when expressing planetary properties as multiples or fractions of a constant terrestrial radius; if the choice between equatorial or polar radii is not explicit, the equatorial radius is to be assumed, as recommended by the [[International Astronomical Union]] (IAU).<ref name="IAU XXIX" />
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)