The magnitude of gravity remains constant at all points along the geoid
the verdict
REFUTED
the evidence says no
confidence 13/100
The magnitude of gravity is not constant across the geoid; it varies due to factors such as mass distribution, Earth's rotation, and local topographic anomalies.
Evidence against · 3
Gravity, Tides, and Topography on Small Satellites and Asteroids: Application to Surface Features of the Martian Satellites
1993 · cited by 117
The study discusses how surface gravity on irregular bodies varies due to gravitational potential, shape, and rotational/tidal effects rather than remaining uniform.
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More against · 2
Understanding curvatures of the equipotential surface in gravity gradiometry
2018 · cited by 5
The analysis of curvatures of equipotential surfaces demonstrates that gravity gradients and local anomalies cause spatial variations along these surfaces.
The Radial Integral of the Geopotential
2025 · cited by 2
The examination of the geopotential and disturbing potential shows spatial patterns and variations across the geoid rather than a constant magnitude of gravity.