Connection coefficients in Earth orbit

In summary, the conversation discusses a problem with exercise 12.6 in the MTW textbook and asks for clarification on the Riemann tensor components and connection coefficients in a primed coordinate system. The conversation also discusses transformations and the effects of Earth's gravity on the coordinate system. Through further analysis, the individual comes to the conclusion that their transformations are correct and that the results for the connection coefficients need to be squared up with the values for the Riemann tensor components.
  • #1
TerryW
Gold Member
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I've run into a couple of problems with exercise 12.6 in MTW (attached).

At this stage, all I'm asking is for someone to give me answers to the following questions:

1. What are the Rα'β'γ'δ' in the primed co-ordinate system? and

2. What are the non-zero connection coefficients in the primed co-ordinate system?

I started with an Earth bound co-ordinate system fixed so that the x-axis runs from the centre of the Earth through the prime meridian at the equator and worked to get the co-ordinate transformations between (x' , y') and (x , y) and used -2GM/R2 for Rα1010 and GM/R2 for R2020. The results for R1'0'1'0' and R2'0'2'0' didn't turn out as I think they should.For my connection coefficients I ended up with

Γ1'0'0' = +ω2x' ,

Γ2'0'0' = -2ω2y'

Γ1'0'2' = -ω

Γ2'0'1' = +ωWhich didn't give a good result for the geodesic equation for y'.

I used the connection coefficients to calculate R1'0'1'0' and Rα2'0'2'0' and ended up with 2ω2 and -ω2 respectively which also doesn't look quite right.Can anyone put me on the right track here?RegardsTerryW
 

Attachments

  • Geodesic Deviation above the Earth.pdf
    1.2 MB · Views: 322
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  • #3
TerryW said:
the co-ordinate transformations between (x' , y') and (x , y)

What transformations did you come up with?

TerryW said:
used -2GM/R2 for Rα1010 and GM/R2 for R2020.

Where did you get these from? They don't look right. Remember that the Riemann tensor describes tidal gravity, not "acceleration due to gravity". (Also, I'm not sure the problem is asking you to take the Earth's gravity into account. See below.)

TerryW said:
For my connection coefficients I ended up with

What did you start with? If you started with the connection coefficients in the unprimed frame being all zero, are you aware that this is only true if we ignore the Earth's gravity? That may indeed be what the problem is asking you to do (I'm not sure), but if so, the Riemann tensor components will also all be zero in the unprimed frame; all of the actual interesting stuff comes from the coordinate transformations.
 
  • #4
PeterDonis said:
What transformations did you come up with?

PeterDonis said:
Where did you get these from? They don't look right. Remember that the Riemann tensor describes tidal gravity, not "acceleration due to gravity". (Also, I'm not sure the problem is asking you to take the Earth's gravity into account. See below.)

First of all, thanks for your reply.

I've written out my transformations and attached them, along with a page from MTW containing the Riemann tensor I used (with the Z and X axes interchanged)

I must say I have tried hard to find examples of Riemann tensor components and Connection Coefficients for this situation on the Internet with no success at all.RegardsTerry W
 

Attachments

  • My transformation and Riemann components.pdf
    2.9 MB · Views: 266
  • #5
TerryW said:
I've written out my transformations and attached them, along with a page from MTW containing the Riemann tensor I used (with the Z and X axes interchanged)

Ok, you had a typo in the OP, you had ##R^2## where it should be ##R^3## in the denominators of the Riemann tensor coefficients, that was what confused me about those. With the typo corrected, those are the right Riemann tensor components in the vicinity of the Earth, if we are including Earth's gravity. But if we are including Earth's gravity, then things get a lot more complicated because space is no longer Euclidean. Your coordinate transformation appears to assume that space is Euclidean, which would mean we are ignoring Earth's gravity and working in an SR inertial frame centered on an idealized "Earth" that has no mass (so "Earth" is really just an identifier for a region of space). If that is the case, then the Riemann tensor components in the unprimed frame are all zero. If it's not, then your coordinate transformation needs to start from Schwarzschild coordinates, not ordinary Cartesian coordinates, in the unprimed frame.

Even if we assume we are ignoring Earth's gravity (which is the easier way to proceed), your coordinate transformation doesn't look right. First, since both coordinate systems are supposed to be Cartesian (x, y, z), you don't need to go through the intermediate step of translating into radius and angular coordinates; that just introduces confusion. You should be able to write down, at a given instant of time, a direct transformation between the x, y, z of the unprimed (non-rotating) coordinates and the x', y', z' of the primed (rotating) coordinates.

Second, note that I said "a given instant of time". The primed coordinates are attached to an object moving in a circle, so the coordinate transformation should have factors in it describing that motion--such as the angular velocity ##\omega##. No such factor appears in what you wrote down.
 
  • #6
Peter,

Thanks for your detailed reply. It prompted me to take a fresh look at the problem and I've spotted something I'd overlooked earlier.

Some of the work in this chapter of MTW is looking at Galilean frames which have the particular characteristic that Γj00 = ∂φ/∂xj, all other Γαβγ = 0 and Rj0k0 = Γj00,k.

This then leads to Γ100,1 = R1010 and Γ200,2 = R2020.

As φ = -GM/R (I need to check out the minus sign, but MTW says that φ = - U (the Newtonian potential) so I think it is OK), then with φ = -GM/(x2+y2)½ then R1010 and R2020 are the same, so the transformation is simple, leading to R1'0'1'0' and R2'0'2'0' being the same as R1010 and R2020 respectively. ( A simple transformation as the problem says!)

(I realize now that the Riemann components I'd been using earlier were incorrect because they represent the components in a local Lorentz frame which isn't the same as my frame fixed at the centre of the earth.)

I feel confident about my transformations at this stage. As you say, they represent a given instance of time, but once you differentiate wrt to time, then d/dt sinθ = cosθdθ/dt, where dθ/dt = ω.

All I need to do now is go through my workings on the results for Γα'β'γ' to see if I can square them up with the values for R1'0'1'0' and R2'0'2'0'.

I'm off on holiday tomorrow so I won't be able to do too much over the next ten days, but I'll drop a post to you when I've reworked everything - hopefully clearing up the issues.
Regards
TerryW
 
  • #7
Hi Peter,
I've made progress while on holiday and I'm a step nearer a consistent set of answers to this problem.
I noticed that I made a transcription error in my 'Transformations' attachment so I've attached a corrected version.
I had a further look at the transformations for R1010 and R2020 and found that they were a bit more complicated, but when I worked through them, the results I got for R1'0'1'0' and R2'0'2'0' were -2GM/R3 and GM/R3 respectively, ie they have the same form as the Riemann tensor components derived in Chapter 1 (which I included in my original attachment). I'm pretty sure that these are correct because they represent the accelerations one would observe between two test particles floating inside an orbiting space station, which is in effect, the same situation as this problem - I also found a paragraph in Chapter 1 which is pretty conclusive on the matter.
I then tried to derive the connection coefficients Γ1'0'0' and Γ2'0'0' using formulae given in the text and which I have derived myself in an earlier exercise. I was hoping the result would give Γ1'0'0' = R1'0'1'0'x and Γ2'0'0' = R2'0'2'0'y, but my results are wide of the mark.

My workings run to several pages but I would really appreciate it if you could take a look at what I have done to see if you can see where it is all going wrong. Would you be willing to do this?RegardsTerryW
 

Attachments

  • My transformation updated.pdf
    215.3 KB · Views: 225
  • #8
TerryW said:
I would really appreciate it if you could take a look at what I have done to see if you can see where it is all going wrong.

I can, but it won't be for several days. I don't currently have access to my copy of MTW, and I would like to review it while I'm looking at what you've done.
 
  • #9
Thanks for this. It will take me a couple of days to write up my workings into a presentable form anyway.

By the way, although I do have my original copy of MTW (bought in the early 70s), I also recently came across a PDF on the internet which is a scan of the entire book. I'll see if I can find the link again for you - I find it useful to have on my iPad and for printing out the odd page when I need it.

Regards

Terry
 
  • #10
TerryW said:
By the way, although I do have my original copy of MTW (bought in the early 70s), I also recently came across a PDF on the internet which is a scan of the entire book. I'll see if I can find the link again for you

I don't think PF rules would permit posting the link here since it's still a copyrighted work.
 
  • #11
Hi Peter,

Here is my write up for the derivation of the connection coefficients.

Many thanks for agreeing to take a look.Regards
TerryW
 

Attachments

  • Finding Connection Coeffients.pdf
    969.7 KB · Views: 237
  • #12
Terry, you have gotten me interested in this problem! I have worked on it off and on for several days and managed to get some results. I might very well have made some errors (including conceptual ones). I hope you and Peter don’t mind if I enter the discussion.

First, I agree with your results for the nonzero components of the Riemann tensor.

However, I don’t agree with your argument for showing that ##R^{1’}_{0’ 1’ 0’}x^{1’} = \Gamma^{1’}_{0’ 0’}##. On the first page of the last set of notes you posted, the geodesic deviation equation doesn’t look correct. The second derivative with respect to lambda should be the covariant second derivative rather than the ordinary second derivative. This will involve some ##\Gamma##’s. See box 12.1 for a similar calculation. But in Box 12.1 the calculation is done in a Galilean coordinate system while in our problem we are working in the non-Galilean system (primed frame) of the orbiting laboratory.

In your expression for the geodesic equation, you have only ##\Gamma^{\alpha}_{0’ 0’}## appearing. But I believe there will be other terms of the form ##\Gamma^{\alpha}_{k’ 0’} \frac{dx^{k’}}{d \lambda}## . However, the solution to the problem will only require using the geodesic deviation equation. The geodesic equation will not be needed.

When you derive the expressions for the ##\Gamma^{k’}_{0’ 0’}## connection coefficients in the rest of your notes, they will only be needed at the origin of the primed frame when using the geodesic deviation equation. So you can set ##x’ = y’ = z’ = 0##. You can see that all of the ##\Gamma^{k’}_{0’ 0’}## terms are zero at the origin. However, some of the ##\Gamma^{j’}_{0’ k’}## are nonzero at the origin and they will occur in the geodesic deviation equation.
 
  • #13
Hi TSny,

Thanks for your thoughts. You are more than welcome to join in.

TSny said:
I have worked on it off and on for several days and managed to get some results. I might very well have made some errors (including conceptual ones).
That's a relief - if you had worked through it in fifteen minutes and reached a consistent answer that I'd missed, I'd feel a bit crushed!

I'll go back to my work and have a think about your comments.

RegardsTerryW
 
  • #14
Suppose you release an object at rest a small distance out along the ##x^{1’}## axis.

The geodesic equation would imply that just after release $$\frac{d^2x^{1’}}{d{ t’}^2}+ \Gamma^{1’}_{0’ 0’} = 0$$ where ##\Gamma^{1’}_{0’ 0’}## is to be valuated at the location of the object.

The geodesic deviation equation will imply that just after release $$\frac{d^2x^{1’}}{d{ t}’^2}+ \left(\Gamma^{1’}_{2' 0’}\Gamma^{2’}_{1’ 0’} + R^{1’}_{0’ 1’ 0’}\right)x^{1'} = 0$$ where the gamma factors come from the covariant derivatives. Here the gammas and R factors are to be evaluated at the origin of the primed frame.

You can check that the two equations are in agreement if you use your results for the values of the ##\Gamma##'s and R’s.
 
  • #15
Hi TSny,

Many thanks for your help with this. Much appreciated.

I agree that my attempt to equate the Riemann components and the Connection Coefficients was a mistake. I can see where I got it from and I just got it wrong!

There were also a couple of things in the question that I missed. One is the quite clear statement that the primed frame is not Galilean, the other is that the question, as you quite rightly point out, asks only for an evaluation of the Connection Coefficients at the origin of the primed frame. (RTFQ!)

I had already evaluated Γ1'0'2' ( = -ω) and Γ2'0'1' ( = ω) and I have used these, in conjunction with Γ1'0'0' and Γ2'0'0' to derive R1'0'1'0', R2'0'2'0' and R1'0'2'0'. They all check out fine!

I'm a bit puzzled by your equation d2x'/dt'2 + (Γ1'0'2'Γ2'0'1' + R1'0'1'0')x1' = 0. Surely the equation is just d2x'/dt'2 + R1'0'1'0'x1' = 0, the geodesic separation equation, isn't it?

The other equation is d2x2'/dt'2 + R2'0'2'0'x2' = 0

These equations would seem to indicate that the bag of rubbish released at a distance y' out in the direction of motion would see the bag slowly approach the space station but if the bag is placed at a distance x' perpendicular to the direction of motion, it will gradually move away from the space station. I have a bit of a problem validating this analysis by examining the Keplerian orbits though. If the rubbish bag is released at a distance x' perpendicular to the direction of motion, assuming it has the same tangential velocity as the space station, it will be traveling too fast for a circular orbit (if it is further from earth) and will therefore move in an elliptical orbit, and although it may move away initially, it will not do so indefinitely as it's elliptical orbit will limit it's maximum distance from the space station. If it is released at a distance y' out in the direction of motion, as it has the same velocity, it will just continue in a circular orbit ahead of the space station. These are just qualitative ideas at the moment, I'm still working on the maths but I would appreciate any thoughts you have.RegardsTerryW
 
  • #16
TerryW said:
I had already evaluated Γ1'0'2' ( = -ω) and Γ2'0'1' ( = ω) and I have used these, in conjunction with Γ1'0'0' and Γ2'0'0' to derive R1'0'1'0', R2'0'2'0' and R1'0'2'0'. They all check out fine!
To get the Riemann components in the primed frame, you don't need to derive them from the connection coefficients. As hinted in the problem statement the primed Riemann coefficients can be obtained by a "trivial transformation of tensorial components". I actually had to spend some time thinking about that, but I believe it's true that it is easy to get the primed components from the unprimed components with virtually no calculation. I'll let you think about that if you want.

I'm a bit puzzled by your equation d2x'/dt'2 + (Γ1'0'2'Γ2'0'1' + R1'0'1'0')x1' = 0. Surely the equation is just d2x'/dt'2 + R1'0'1'0'x1' = 0, the geodesic separation equation, isn't it?
No. This is a good exercise in carrying out covariant differentiation. To avoid possible confusion, I think it is a good idea to use the notation ##n^k## for the spatial components of the deviation vector that measures the deviation between the "fiducial" geodesic and the neighboring geodesic of the object of interest (or "test particle"). The fidcuial geodesic in our problem is the geodesic of the center of the freely falling space laboratory. That is, it is the geodesic along which the origin of the primed coordinate system is moving. So, the "tail" of ##n^k## will always be at the origin of the primed system and the "head" of ##n^k## will be at the location of the test particle.

The covariant derivative as written in the middle of Box 12.1 is: $$\frac{Dn^k}{dt} = \frac{dn^k}{dt} + \Gamma^k_{\beta \mu} n^{\beta}\frac{dx^\mu}{dt}$$ For convenience, I will drop all primes since it is understood that we are working now exclusively in the primed frame. In the above equation, the gammas are evaluated on the fiducial geodesic at the location of the tail of ##n^k## and, hence, at the origin of the primed coordinate system. This is why we only need the gammas at the origin. The ##\frac{dx^\mu}{dt}## factor is the time derivative of ##\mu##th coordinate of the point on the fiducial geodesic corresponding to the tail of ##n^k##. But since we are working in the primed system, we always have ##x^k = 0## and ##x^0 = t##. Thus, see what you get for ##\frac{Dn^1}{dt}## and ##\frac{Dn^2}{dt}## keeping in mind that most of the gammas are zero. Then you can go on to try to get the second covariant derivatives.

These equations would seem to indicate that the bag of rubbish released at a distance y' out in the direction of motion would see the bag slowly approach the space station but if the bag is placed at a distance x' perpendicular to the direction of motion, it will gradually move away from the space station. I have a bit of a problem validating this analysis by examining the Keplerian orbits though. If the rubbish bag is released at a distance x' perpendicular to the direction of motion, assuming it has the same tangential velocity as the space station, it will be traveling too fast for a circular orbit (if it is further from earth) and will therefore move in an elliptical orbit, and although it may move away initially, it will not do so indefinitely as it's elliptical orbit will limit it's maximum distance from the space station. If it is released at a distance y' out in the direction of motion, as it has the same velocity, it will just continue in a circular orbit ahead of the space station. These are just qualitative ideas at the moment, I'm still working on the maths but I would appreciate any thoughts you have.
Yes, if the bag is released from rest at a small distance along the y' axis, then it should essentially stay at that point in the primed frame. Once you get the correct differential equation for ##n^2## you will see that this is the case.

And, yes, if the bag is released from rest at a positive value of x', then it should initially start moving farther away from the origin. This will be validated by the correct differential equation for ##n^1##.
 
  • #17
Hi again TSny,

You really are doing sterling work on my behalf!

TSny said:
To get the Riemann components in the primed frame, you don't need to derive them from the connection coefficients.

I know this is the case and I'd done that. I just thought it would be fun to see if deriving Riemann from the Connection Coeffs and their derivatives would work and it did.

TSny said:
but I believe it's true that it is easy to get the primed components from the unprimed components with virtually no calculation. I'll let you think about that if you want.

Yes, I can see how - just put θ = 0 in my transformation! I did this originally but I was worried about the fact that I seemed to be choosing a rotating frame, but as the process does not involve any derivatives of the Aj'k terms, no problems arise.

TSny said:
Then you can go on to try to get the second covariant derivatives.

I've worked this through and got to:
$$\frac{d^2n^{1}}{dt^2} = \Gamma^1_ { 02}\Gamma^2_ { 01} n^1 = R^1_ { 010}n^1$$

and
$$\frac{d^2n^{2}}{dt^2} = \Gamma^2_ { 01}\Gamma^1_ { 02} n^1 = R^2_ { 020}n^2$$

Using my results for ##\Gamma^2_ { 01}## and ##\Gamma^1_{02}##, I get
$$\frac{d^2n^{1}}{dt^2} = 3\omega^2n^1$$ and
$$\frac{d^2n^{2}}{dt^2} =0$$

So the bag placed further out on the x' axis moves away and there is no acceleration along the y' axis.

So this agrees with you and my earlier Keplerian consideration but it doesn't fit with MTW page 29, which in §1.6 states that in orbit around the earth, the two particles will move towards each other.

Is this one of the legendary 2 mistakes? I know the usual argument is that there is a tiny angle between the gravitational force vectors acting on the two particles which results in a tiny force of attraction and I can see how this would manifest itself if the spaceship was falling radially inward towards the centre of the earth. But in orbital motion, the radial gravitational forces are providing the inward accelerations which maintain circular orbits which will have exactly the same period of motion - no change in separation.

Do you think I've cracked this now (with your much appreciated help of course)? And how do I give you a big 'like"?Regards

TerryW
 
  • #18
TerryW said:
Hi again TSny,
I've worked this through and got to:
$$\frac{d^2n^{1}}{dt^2} = \Gamma^1_ { 02}\Gamma^2_ { 01} n^1 = R^1_ { 010}n^1$$

and
$$\frac{d^2n^{2}}{dt^2} = \Gamma^2_ { 01}\Gamma^1_ { 02} n^1 = R^2_ { 020}n^2$$

Using my results for ##\Gamma^2_ { 01}## and ##\Gamma^1_{02}##, I get
$$\frac{d^2n^{1}}{dt^2} = 3\omega^2n^1$$ and
$$\frac{d^2n^{2}}{dt^2} =0$$

OK. ( I'm sure you meant to type "+" instead of "=" in front of the last terms on the right in the first two equations.) The above equations hold at an instant when the bag is at rest near the origin in the primed frame. So, they tell us how the bag will initially begin to move just after being released at rest. However, when the bag is moving (as in the problem where the bag is jettisoned from the origin), there are additional Coriolis terms that involve the first time derivatives of ##n_1## or ##n_2##.

So the bag placed further out on the x' axis moves away and there is no acceleration along the y' axis.

So this agrees with you and my earlier Keplerian consideration but it doesn't fit with MTW page 29, which in §1.6 states that in orbit around the earth, the two particles will move towards each other.

Is this one of the legendary 2 mistakes? I know the usual argument is that there is a tiny angle between the gravitational force vectors acting on the two particles which results in a tiny force of attraction and I can see how this would manifest itself if the spaceship was falling radially inward towards the centre of the earth. But in orbital motion, the radial gravitational forces are providing the inward accelerations which maintain circular orbits which will have exactly the same period of motion - no change in separation.
I'm not familiar with the "2 legendary mistakes". It would be interesting to know what they are. But, it does seem to me that they made a gaffe here. Certainly, as you say, two orbiting test particles of negligible mass on the same circular orbit would maintain constant separation.
 
  • Like
Likes TerryW
  • #19
Hi TSny

TSny said:
I'm sure you meant to type "+" instead of "=" in front of the last terms on the right in the first two equations.)

Yes, it is a typo.

Looking back at some of my original post, I actually did have the answer (for Γ100 and Γ200) but then tried to reconcile these answers with MTW §1.6, which we now agree is wrong.

However, I think I learned quite a lot from following your guidance so thanks again for your help.

TSny said:
I'm not familiar with the "2 legendary mistakes". It would be interesting to know what they are.

I can recall seeing this somewhere in the past but I haven't been able to find the reference again today. I believe it was one of the authors who said it but, tantalisingly, didn't reveal what the mistakes were.

Anyway, on to Chapter 14, (I've done all the problems on Ch 13!)RegardsTerryW
 
  • #20
OK. Sounds good. Enjoy chapter 14. The book is truly amazing. Seems like people either love it or hate it. Yesterday, I ran across this interesting article related to the initial publication of the book: http://www.jstor.org/stable/10.1086/664983
 
  • #21
TerryW said:
MTW §1.6, which we now agree is wrong.

"Wrong" is a bit strong. It's true that the words "in orbit" are used, which is evidently a typo or a bad choice of terminology. But the ensuing discussion is correct if we reinterpret "in orbit" to mean, not "in a circular orbit" but "freely falling towards the Earth". If a pair of test particles free-falling towards the Earth is separated radially, their separation will increase; if they are separated tangentially, their separation will decrease. This is clearly what the rest of this section is describing. In other words, the (unstated) assumption in the rest of the discussion is that the pair of test particles is initially at rest relative to the Earth.

That said, we can also consider what would happen if we ran an experiment inside a spacecraft in a perfectly circular orbit, and placed a pair of test objects initially at rest relative to each other (and the spacecraft ). If the two test objects are separated radially (i.e., along a radial line through the center of the Earth, one slightly further than the other), then the lower one will be moving slightly too slow for a circular orbit at its altitude, and will slowly lose altitude--i.e., its actual orbit will be elliptical, with its starting point as apogee. It will also slowly move forward relative to the spaceship, because the orbital period of its actual orbit will be slightly shorter than that of the spacecraft . The higher object, conversely, will be moving slightly too fast for a circular orbit at its altitude, and will slowly gain altitude--its actual orbit will be elliptical, with its starting point as perigee. It will also slowly move backward relative to the spaceship, because its new orbital period will be slightly longer than that of the spacecraft . So the separation vector between the two test objects will both lengthen and rotate relative to the spacecraft .

If the two test objects are separated tangentially, at exactly the same altitude as the center of mass of the spacecraft , then yes, their separation vector will remain constant, relative to the spacecraft (because they are both in circular orbits of exactly the same altitude as the spacecraft ). But the MTW discussion in section 1.6 is clearly not contemplating this kind of situation (despite the use of the words "in orbit", as above), because it doesn't talk about the rotation of the radial separation vector (per the above) at all.
 
  • #22
Peter, I agree that if one interprets the phrase "in orbit about the earth" to mean freely falling directly toward the earth, then there would be no problem. But I believe that most readers would not interpret it this way based on how "orbit about" is used in other parts of the chapter, such as the last paragraph on page 23. However, as you say, they apparently had in mind a frame falling directly toward the earth. The Newtonian equations (1.5) would not apply to a local frame carried by an orbiting spaceship.

You have a nice description of what does happen in the frame of an orbiting spaceship.
 
  • #23
Hi TSny and PeterDonis,

TSny said:
But I believe that most readers would not interpret it this way based on how "orbit about" is used in other parts of the chapter, such as the last paragraph on page 23

It may not be what they meant, but it is certainly the way I read it! TerryW
 
  • #24
Hi TSny,

I enjoyed reading the article at the end of your link!

Regards

TerryW
 
  • #25
TerryW said:
It may not be what they meant

I suspect the phrase "in orbit" was a typo (or maybe a "thinko"?) in that particular section, since, as we've noted, the context makes it clear that the scenario being envisioned is a pair of test objects free-falling towards the Earth.
 

Related to Connection coefficients in Earth orbit

1. What are connection coefficients in Earth orbit and why are they important?

Connection coefficients in Earth orbit, also known as geopotential coefficients, are numerical values used to describe the Earth's gravitational field. They are important because they provide information about the Earth's shape and mass distribution, which is crucial for understanding orbital dynamics and predicting the movement of objects in Earth orbit.

2. How are connection coefficients determined?

Connection coefficients are determined through satellite missions, such as the Gravity Recovery and Climate Experiment (GRACE), which measure the Earth's gravity field. These measurements are then used to calculate the coefficients using mathematical models and algorithms.

3. What is the relationship between connection coefficients and Earth's geoid?

The geoid is a representation of the Earth's shape, taking into account its irregularities and variations in gravity. Connection coefficients are used to define the geoid, as they provide information about the Earth's gravity field and therefore its shape.

4. How do connection coefficients affect satellite orbits?

Connection coefficients play a significant role in determining the orbital paths of satellites. They affect the gravitational pull on a satellite and can cause variations in its orbit. This is important for satellite operations and trajectory planning.

5. Are connection coefficients constant or do they change over time?

Connection coefficients are not constant and can change over time due to factors such as the Earth's rotation and changes in the Earth's mass distribution. Scientists continuously monitor and update these coefficients to improve our understanding of the Earth's gravitational field.

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