
The variation of gravitational acceleration (g) on Earth is mostly influenced by the fact that Earth is not a perfect sphere — it is slightly flattened at the poles and bulged at the equator, so a point on the equator is farther from the center of gravity. Since the gravitational field weakens with distance, the gravitational force on objects located at the equator is smaller. Because of this alone, g is 0.18% smaller at the equator than at the poles.





