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geoid

American  
[jee-oid] / ˈdʒi ɔɪd /

noun

  1. an imaginary surface that coincides with mean sea level in the ocean and its extension through the continents.

  2. the geometric figure formed by this surface, an ellipsoid flattened at the poles.


geoid British  
/ ˈdʒiːɔɪd /

noun

  1. a hypothetical surface that corresponds to mean sea level and extends at the same level under the continents

  2. the shape of the earth

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

geoid Scientific  
/ jē′oid′ /
  1. The hypothetical surface of the Earth that coincides everywhere with mean sea level and is perpendicular, at every point, to the direction of gravity. The geoid is used as a reference surface for astronomical measurements and for the accurate measurement of elevations on the Earth's surface.


Other Word Forms


Etymology

Origin of geoid

First recorded in 1880–85, geoid is from the Greek word geoeidḗs earthlike. See geo-, -oid


Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

See Examples For:

Forte also claimed the computer simulations did not accurately project the actual shape of Earth as a geoid.

From Salon ● Jul. 26, 2023

These plumes, along with the nearby mantle structure, are believed to form the "gravity" hole because it winds up being the lowest point in that geoid, creating its biggest gravitational anomaly.

From Salon ● Jul. 26, 2023

“When the temperature anomalies causing this low geoid shift out of the present-day location,” Pal says, “the geoid low will start to dissipate.”

From Scientific American ● Jun. 26, 2023

This produces an exaggerated visualization of our planet’s gravitational high and low spots called the global geoid.

From Scientific American ● Jun. 26, 2023

In 1849, Stokes derived a theorem whereby the distance N of the geoid from the ellipsoid of reference can be obtained from an integration of gravity anomalies over the surface of the earth.

From Development of Gravity Pendulums in the 19th Century Contributions from the Museum of History and Technology, Papers 34-44 On Science and Technology, Smithsonian Institution, 1966 by Victor Fritz Lenzen

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