Variation of gravitation field strength?

AI Thread Summary
The gravitational field strength (g) varies across the Earth's surface, primarily due to its shape as an oblate spheroid rather than a perfect sphere. At the equator, there is less mass beneath a person compared to the North Pole, affecting the gravitational pull experienced. Additionally, the Earth's rotation influences weight measurements at the equator, but this effect is typically not included in calculations of g. Understanding these factors clarifies why g is not uniform across the planet. Overall, the variation in gravitational strength is a result of both distance from the Earth's center and the distribution of mass.
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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