Normal gravity is the gravity of a model Earth: an ellipsoid of revolution with the Earth’s mass and rotation, chosen so that its surface is an equipotential of its own gravity (gravitation plus the centrifugal effect). On that surface, normal gravity depends on latitude alone.
উদাহরণ
Example 11.12 (A station in the hills)
At a station at latitude and above sea level, the gravimeter gives . Normal gravity there is ; the measured value is lower by . The free-air correction is , so . The Bouguer correction is , so : there is less mass below this station than below a station at sea level, once the rock above sea level is removed.