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First off, **altitude** plays a role. As you move further away from the center of the Earth (i.e., higher altitude), the gravitational force decreases. This means that 'g' will be slightly lower at the top of a mountain than at sea level. The difference is usually quite small, but it's measurable with sensitive equipment. Secondly, **latitude** has an effect. The Earth isn't a perfect sphere; it bulges slightly at the equator. This means that the distance from the center of the Earth is greater at the equator than at the poles. Additionally, the Earth rotates, which creates a centrifugal force that slightly reduces the effective gravitational pull at the equator. As a result, 'g' is slightly lower at the equator and slightly higher at the poles. The difference is relatively small, but it's a significant factor in precise scientific measurements.
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