geoid

/ˈdʒiːɔɪd/
noun
  1. The shape that the surface of the Earth's oceans would take if they were not disturbed by tides, winds, or currents, used as a model for measuring the Earth's true shape.
    • The geoid is not a perfect sphere because gravity varies across the planet.
    • Scientists use the geoid to calculate precise elevations on land.
    • GPS devices rely on the geoid model to give accurate altitude readings.
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