Estimating Flattening of the Earth

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SUMMARY

The discussion focuses on estimating the flattening of the Earth using the formula 1 - RP/RE, where RP is the polar radius and RE is the equatorial radius. The solution involves approximating the Earth as an oblate spheroid and applying Newton's law of gravity. The final expression derived for the flattening is 1 - RP/RE ≈ 3ω2/(8Gπρ), where ω is the angular velocity, G is the gravitational constant, and ρ is the density of the Earth. The discussion concludes with a suggestion to calculate ω using T, the period of one rotation of the Earth, and to look up the mass of the Earth for accurate results.

PREREQUISITES
  • Understanding of basic physics concepts, particularly Newton's law of gravity.
  • Familiarity with the properties of oblate spheroids.
  • Knowledge of angular velocity and its calculation.
  • Basic understanding of gravitational constants and Earth's density.
NEXT STEPS
  • Calculate the angular velocity of the Earth using the formula ω = 2π/T, where T is the rotation period.
  • Research the gravitational constant (G) and its significance in gravitational calculations.
  • Look up the mass of the Earth for use in flattening calculations.
  • Explore the implications of Earth's flattening on geodesy and satellite navigation.
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Students and professionals in physics, geophysics, and engineering, particularly those interested in geodesy, planetary science, and Earth measurements.

Fightfish
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Homework Statement
Estimate the flattening of the earth, given by [tex]1 - \frac{R_{P}}{R_{E}}[/tex], where [tex]R_{P}[/tex] is half the distance between the north pole and south pole and [tex]R_{E}[/tex] the radius of the equator.

The attempt at a solution
Well, I did manage to obtain a solution of sorts, but it involved a lot of approximations along the way, which I am not sure if they are all justifiable.

We start off with the base assumption that the flattening of the Earth is very small, such that there is relatively little deviation from a spherical shape.
Then, Newton's law of gravity is approximately true for this oblate spheroid. Modeling the Earth as a frictionless incompressible fluid, in order for a point at the pole surface to be in hydrostatic equilibrium with one at the equatorial surface, we have:
[tex]\frac{GM}{R_{P}^{2}} = \frac{GM}{R_{E}^{2}} + R_{E} \omega^{2}[/tex]
[tex]\frac{R_{E}^{2}}{R_{P}^{2}} = 1 + \frac{R_{E}^{3} \omega^{2}}{GM}[/tex]​

Now, if the Earth were a perfect sphere, [tex]M = \frac{4}{3}\pi R_{S}^{3} \rho[/tex]. Since the flattening of the Earth is very small, we expect [tex]\frac{R_{E}^{3}}{R_{S}^{3}} \approx 1[/tex]. Then,
[tex]\frac{R_{P}}{R_{E}} = (1 + \frac{3 \omega^{2}}{4G\pi\rho})^{-\frac{1}{2}}[/tex]​

As we expect [tex]\frac{R_{E}}{R_{P}}[/tex] to be very close to 1, this implies that [tex]\frac{3 \omega^{2}}{4G\pi\rho} \ll 1[/tex], and hence
[tex]\frac{R_{P}}{R_{E}} \approx 1 - \frac{3 \omega^{2}}{8G\pi\rho}[/tex]​

Thus, the flattening of the earth
[tex]1 - \frac{R_{P}}{R_{E}} \approx \frac{3 \omega^{2}}{8G\pi\rho} = \frac{3 \pi}{2GT^{2}\rho}[/tex]​

Does this look reasonable?
 
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Fightfish said:
Estimate the flattening of the earth, given by [tex]1 - \frac{R_{P}}{R_{E}}[/tex], where [tex]R_{P}[/tex] is half the distance between the north pole and south pole and [tex]R_{E}[/tex] the radius of the equator.

...
[tex]\frac{R_{E}^{2}}{R_{P}^{2}} = 1 + \frac{R_{E}^{3} \omega^{2}}{GM}[/tex]

I would stop right there. You can work out [itex]\omega = 2\pi/T[/itex] (T = period of one rotation of the earth) and you can look up M (= mass of the earth). There is no need to make any approximations as you have done.

AM
 

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