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Gravity doesn't remain constant across different locations on Earth and changes based on several factors. These variations can happen due to changes in elevation, latitude, and local geological structures. When you are above or below the Earth's surface, the gravitational pull could be weaker or stronger, respectively.
- **Above the surface**: Higher altitudes, such as those experienced in high mountains or airplanes, mean you are further from Earth's center. Here, gravity weakens and you weigh a tiny bit less.
- **Below the surface**: When you dig deeper into Earth, you get closer to the massive central core. As a result, gravity can become stronger because there is more mass above you exerting a pull.

Understanding these gravity variations helps explain why certain locations on Earth have slightly different gravitational forces. This is crucial for applications in geophysics and engineering.

The radius of Earth is an essential parameter for calculating gravitational acceleration. Earth's average radius is approximately 6400 kilometers. This value is fundamental for applying the gravitational formula to predict how gravity changes with altitude and depth.
- At **sea level**, the radius is typically measured from the center of Earth to that point on the surface.
- When you travel **above** the surface, the radius becomes the distance from Earth's center to the point of interest above the surface.
- Similarly, **under the surface**, the radius still extends from the center to where you are below the surface level.

Using Earth's radius in our calculations helps determine how the gravitational force diminishes with height or increases with depth. This knowledge is utilized by scientists and engineers in fields such as satellite launching and underground exploration.

Gravitational formulas play a vital role in evaluating how gravity differs with position relative to Earth. The two key formulas are for calculating gravity above and below the surface.

### Above the SurfaceThe formula to calculate gravity above the surface is \[ g_h = g_0 \left(\frac{R}{R+h}\right)^2 \] where:

• \(g_h\) is the gravity at height \(h\)
• \(g_0\) is the gravity at Earth's surface
• \(R\) is Earth's radius, and
• \(h\) is the height above the surface

This shows that as height increases, gravity decreases.

### Below the SurfaceWhen you're below the surface, gravity is computed using the formula:\[ g_d = g_0 \left(1 - \frac{d}{R} \right) \] with:

• \(g_d\) as gravity at depth \(d\)
• \(g_0\) as surface gravity
• \(d\) as depth beneath the surface

Here, as the depth increases, the gravitational force becomes a function of how close you are to the center through the depth fraction.By understanding these formulas, students can better visualize how gravitational force changes around Earth, enhancing comprehension in physics.