How Does Your Weight Change from the Poles to the Equator?

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    Centrifugal Gravity
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SUMMARY

The weight of an object varies between the poles and the equator due to the Earth's rotation and its shape. An object with a mass of 80 kg experiences a gravitational acceleration of 9.789 m·s−2 at the equator and 9.832 m·s−2 at the poles. This results in a weight difference, where the centrifugal effect at the equator slightly counteracts gravitational pull, while the poles experience a stronger gravitational force due to the Earth's equatorial bulge and flattened shape. Density variations also contribute to local differences in gravitational acceleration.

PREREQUISITES
  • Understanding of gravitational acceleration and its measurement
  • Familiarity with the concepts of centrifugal force and its effects
  • Knowledge of Earth's shape, including equatorial bulge and polar flattening
  • Basic physics principles related to mass and weight
NEXT STEPS
  • Research the effects of centrifugal force on weight at different latitudes
  • Explore the implications of Earth's equatorial bulge on gravitational measurements
  • Study variations in local gravity using tools like gravimeters
  • Investigate density variations in Earth's crust and their impact on gravity
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Physicists, geophysicists, students studying Earth sciences, and anyone interested in the effects of Earth's rotation on weight and gravity.

georgert
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If I have a mass of 80 kg, what would the difference in my weight be at either the North or South Pole and at the equator? It would seem to me that the spin of the Earth would induce a centrifugal effect that would counter somewhat Earth's gravitational pull at the equator, but not do so at Earth's axis of spin.
 
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georgert said:
If I have a mass of 80 kg, what would the difference in my weight be at either the North or South Pole and at the equator? It would seem to me that the spin of the Earth would induce a centrifugal effect that would counter somewhat Earth's gravitational pull at the equator, but not do so at Earth's axis of spin.
That's absolutely correct.
The effects of having an equatorial bulge and flattened poles also contributes to variation of the local value of "g", compared to what you'd get by a strictly spherical shape.
"g" is also slightly dependent upon density variations.


According to Wikipedia, the local values of "g" are as follows:
local gravity, g, increases from 9.789 m·s−2 at the equator to 9.832 m·s−2 at the poles.[1]
 

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