Experimental measurements of gravity can differ from the standard 9.8 m/s² due to various factors, including altitude, distance from the Earth's center, and local geological composition. The acceleration due to gravity decreases slightly with increased distance from the center of the Earth and varies between the poles and the equator, with a difference of about 0.4%. Additionally, experimental errors, air resistance, and friction can significantly impact measurements, often overshadowing the inherent variations in gravitational strength. The Earth's rotation also affects gravity, as centrifugal force counteracts gravitational pull, particularly at the equator. Overall, these factors contribute to the discrepancies observed in experimental gravity measurements.