This value is often rounded to 9.8 m/s² or even 10 m/s² for simpler calculations.
It's important to note that the actual value can vary slightly depending on factors like:
* Altitude: Gravity decreases slightly as you move further away from the Earth's surface.
* Latitude: The Earth is not perfectly spherical, so the value of gravity is slightly higher at the poles than at the equator.
* Local geological variations: The density of the Earth's crust can also affect the local gravitational acceleration.
