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Variations for acceleration due to gravity?
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Variations for acceleration due to gravity?
Understanding Variations in Acceleration Due to Gravity
The acceleration due to gravity (g) is not constant across the Earth's surface. Several factors contribute to its variations.
Factors Affecting Acceleration Due to Gravity
  • Altitude: As altitude increases, the distance from the Earth's center increases, resulting in a decrease in gravitational pull. Thus, g is lower on mountains than at sea level.
  • Latitude: The Earth's shape is an oblate spheroid, causing variations in g based on latitude. It is slightly weaker at the equator due to the centrifugal force from the Earth's rotation and stronger at the poles.
  • Local Geological Structures: The presence of mountains, valleys, and geological formations can cause local variations in g. Denser materials, like minerals and ores, increase gravitational pull, while less dense materials decrease it.
  • Earth's Rotation: The rotation of the Earth affects the perceived acceleration due to gravity. The centrifugal force generated by this rotation counteracts gravitational force, making g slightly less at the equator compared to the poles.


Mathematical Representation
The formula for gravitational force is given by:
  • g = G * (M / r²) where:

    • G: Universal gravitational constant
    • M: Mass of the Earth
    • r: Distance from the Earth's center



This formula illustrates how changes in distance (r) due to altitude or latitude can lead to variations in g.
Understanding these factors is crucial for studies in physics, engineering, and geosciences, as they affect calculations involving motion and forces on Earth.
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Variations for acceleration due to gravity?
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