However, it's important to note that this value is an average and can vary slightly depending on factors such as:
* Latitude: Gravity is slightly weaker at the equator than at the poles due to the Earth's rotation.
* Altitude: Gravity decreases with increasing altitude.
* Local geological formations: Dense rock formations can cause local variations in gravity.
For most practical purposes, the average value of 9.81 m/s² is sufficient.
