Variation of gravitation field strength?

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SUMMARY

The gravitational field strength (g) at the equator is not uniform due to the Earth's shape as an oblate spheroid rather than a perfect sphere. This results in variations in gravitational force because there is less mass between an observer's feet and the Earth's center at the North Pole compared to the Equator. Additionally, while the Earth's angular momentum affects measurements at the equator, it is not included in the calculations of g. Understanding these factors is crucial for accurate physics applications.

PREREQUISITES
  • Understanding of gravitational field strength and its calculations
  • Knowledge of Earth's shape and its implications (oblate spheroid)
  • Familiarity with angular momentum and its effects on measurements
  • Basic physics concepts related to mass and density
NEXT STEPS
  • Research the effects of Earth's shape on gravitational field strength
  • Study the principles of angular momentum in physics
  • Learn about the differences between gravitational acceleration at various latitudes
  • Explore advanced topics in gravitational physics and their practical applications
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Students of physics, educators explaining gravitational concepts, and anyone interested in the nuances of gravitational field strength variations across different geographical locations.

quantumtron
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Hi all, this will be my first physics qns:D more to come...

I just learned that value of g at the equator is not exactly equal to the gravitational field strength. Can anyone explain with workings? i don't really understand my teacher workings.
Also can i clarify if

-We're assuming Earth is perfectly sphere hence Radius (r) is same throughout and Angular speed is the same throughout the earth?

*i suspect there is a printing error on my notes which makes cause my confusion over the understanding of this part hence getting some other people's workings ...
 
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IF the Earth were a perfect sphere, then g would have the same value at any point on its surface. In fact, though, the Earth is an oblate spheroid. In practical terms, this means there is less mass between your feet and the center of the Earth when you stand at the North Pole than when you stand at the Equator. This need not work out to a higher g on the equator--it's a question of distance as well as mass, so density figures in--but in our case, it does.

The Earth's angular momentum will have a marginal effect on your scale if you are weighing something at the Equator, but it is important to note that this dynamic factor is NOT considered when calculating g.
 

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