Explaining Variations of Free-Fall Gravity on Earth?

In summary, according to the data on the Nasa website, the variation in gravitational acceleration around Earth, the Moon, and other planets is due to thermal vectors in the liquid areas of the Earth. If the Lava Lamp Theory were to be correct, at what speed should we be able to observe these changes?
  • #1
StarHunter
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TL;DR Summary
Explaining Earth's changing gravity at sea level or independent of altitude, latitude or lunar influence.
I stumbled upon gravitational variations that do not coincide with altitude, latitude or lunar interference. The only logical explanation I have for this would be the geology or makeup of the earth below those locations. But what is the variation of the Earths makeup below the crust? From my understanding it is fairly homogenous at least at specific depths/locations going to the core. So, if most of the geological variation is on the crust, I don't believe the crust could cause +-0.1m/s variation in the acceleration field. Another theory I had would be thermal vectors in the liquid areas of the Earth obstructing the density layers (lava lamp theory) that would take place without them and in turn would create a more stable and consistent acceleration field. If the Lava Lamp Theory were to be correct, at what speed should we be able to observe these changes?

https://www.britannica.com/science/...ation-around-Earth-the-Moon-and-other-planets
https://www.earthdata.nasa.gov/learn/sensing-our-planet/matter-in-motion-earths-changing-gravity

Thank you
 
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  • #2
StarHunter said:
I stumbled upon gravitational variations that do not coincide with altitude, latitude or lunar interference.
Do you mean things described in the articles you reference?
 
  • #3
PeterDonis said:
Do you mean things described in the articles you reference?
No, they were used as a reference. Moreso explaining Earth's changing gravity at sea level or independent of altitude, latitude or lunar influence.
 
  • #4
StarHunter said:
No, they were used as a reference.
Then where did you "stumble on" these variations you claim?
 
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  • #5
PeterDonis said:
Then where did you "stumble on" these variations you claim?
Data is on the Nasa website.
 
  • #7
StarHunter said:
Data is on the Nasa website.
Data for what? I see no calculations in your OP.
 
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  • #8
StarHunter said:
How does this relate to the claims you make in your OP?

You should be aware that personal theories and personal speculations are off limits here at PF. Your OP looks like personal theories and personal speculations.
 
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  • #9
PeterDonis said:
How does this relate to the claims you make in your OP?

You should be aware that personal theories and personal speculations are off limits here at PF. Your OP looks like personal theories and personal speculations.
I did not see that anywhere and I find that hard to believe as that is a key function of a forum. Math and science are ever evolving, and I have seen countless posts and threads where theory is discussed. At the end of the day I was looking for an explanation of an observed phenomenon. I don't think that is off limits...
 
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  • #10
StarHunter said:
I did not see that anywhere
It's right there in the rules that you signed up to:

Greg Bernhardt said:
Generally, in the forums, we do not allow the following:
  • Discussion of theories that appear only on personal websites, self-published books, etc.
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StarHunter said:
I find that hard to believe as that is a key function of a forum
Not this one. PF is for helping people to understand mainstream science, not for speculating.

StarHunter said:
At the end of the day I was looking for an explanation of an observed phenomenon. I don't think that is off limits...
It isn't. But claims like this in your OP are not doing that:

StarHunter said:
I don't believe the crust could cause +-0.1m/s variation in the acceleration field
StarHunter said:
Another theory I had would be thermal vectors in the liquid areas of the Earth obstructing the density layers (lava lamp theory) that would take place without them and in turn would create a more stable and consistent acceleration field.
 
  • #11
PeterDonis said:
It's right there in the rules that you signed up to:

Not this one. PF is for helping people to understand mainstream science, not for speculating.It isn't. But claims like this in your OP are not doing that:
I was suggesting potential answers that ARE mainstream that I may be unaware of. As for the theories aspect, I will refrain from that in the future. I was looking for a productive discussion and your hostility is not adding anything constructive.
 
  • #12
StarHunter said:
So, if most of the geological variation is on the crust, I don't believe the crust could cause +-0.1m/s variation in the acceleration field.
Apparently it's enough that you'll weigh less here in the Great White North than among our neighbors to the south. (About a tenth of a ounce less, but still...)

https://www.cntraveler.com/stories/2014-04-14/the-laurentide-ice-sheet-maphead
 
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  • #13
StarHunter said:
At the end of the day I was looking for an explanation of an observed phenomenon
That observed phenomenon, I presume, being the variation of acceleration due to gravity? The articles you referenced already do a good job of explaining where that comes from. Is there something in them that you are having trouble understanding?

StarHunter said:
gravitational variations that do not coincide with altitude, latitude or lunar interference.
Those are very small, about one part in a million according to the articles you reference. That's much smaller than the ##0.1## m/s^2 amount that you appear to find questionable (and it's not clear where you are getting that number from); one part in a million is about ##0.00001## m/s^2.
 
  • #14
StarHunter said:
I was suggesting potential answers that ARE mainstream that I may be unaware of.
If they are mainstream, you should be able to give mainstream references for them. I am not aware of any mainstream reference for "Lava Lamp Theory" in this domain, but if you are, please give it.

I see no other suggested answer in your post, just doubt about a number, ##0.1## m/s^2, that I can't find in any of your references so I don't know where you got it from. And, as I've noted, it's several orders of magnitude larger than the number given in your references.
 
  • #15
StarHunter said:
I was looking for a productive discussion
The best way to start one is to correctly describe what the references you are relying on actually say.

StarHunter said:
your hostility is not adding anything constructive.
Enforcement of the rules is not hostility. It's my job as a moderator.
 
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  • #16
PeterDonis said:
That observed phenomenon, I presume, being the variation of acceleration due to gravity? The articles you referenced already do a good job of explaining where that comes from. Is there something in them that you are having trouble understanding?Those are very small, about one part in a million according to the articles you reference. That's much smaller than the ##0.1## m/s^2 amount that you appear to find questionable (and it's not clear where you are getting that number from); one part in a million is about ##0.00001## m/s^2.
You are correct, in consequence any measured variation in general only deviates +-0.0698m/s^2. At least as measured with GRACE (https://www2.csr.utexas.edu/grace/publications/).

Even looking visually.

As far as my initial reference, ""Because the distribution of materials deep inside the Earth varies, its gravity field has hills and valleys. The ocean tries to lay along that hilly surface," said Michael Watkins, GRACE project scientist" and "The Earth's gravity field changes from one month to the next mostly due to the mass of water moving around on the surface,". Again that would come back to my initial question. At what level would the geology changes occur and why are they occurring. I would infer that it would be thermal vectors?
 
  • #17
StarHunter said:
You are correct, in consequence any measured variation in general only deviates +-0.0698m/s^2
Where does this number come from? (A link to a page that just lists a bunch of publications is not a valid reference for a specific claim.) It's quite a bit larger than one part per million.

StarHunter said:
At what level would the geology changes occur and why are they occurring.
All of the references you give mention the Earth's crust.

StarHunter said:
I would infer that it would be thermal vectors?
This is where you get into speculation again, unless you can give a reference for what "thermal vectors" are and why they might be relevant.
 
  • #18
DaveC426913 said:
Apparently it's enough that you'll weigh less here in the Great White North than among our neighbors to the south. (About a tenth of a ounce less, but still...)

https://www.cntraveler.com/stories/2014-04-14/the-laurentide-ice-sheet-maphead
Thats interesting but I don't understand the explanation as with the ground "springing back" the density would decrease but the mass would stay the same or even increase with more water in the ground. I may be very wrong.
 
  • #19
PeterDonis said:
Where does this number come from? (A link to a page that just lists a bunch of publications is not a valid reference for a specific claim.) It's quite a bit larger than one part per million.All of the references you give mention the Earth's crust.This is where you get into speculation again, unless you can give a reference for what "thermal vectors" are and why they might be relevant.
"The acceleration g varies by about 1/2 of 1 percent with position on Earth’s surface, from about 9.78 meters per second per second at the Equator to approximately 9.83 meters per second per second at the poles." In OP Britannica reference.

and
"Gravity on the Earth's surface varies by around 0.7%, from 9.7639 m/s2 on the Nevado Huascarán mountain in Peru to 9.8337 m/s2 at the surface of the Arctic Ocean.[6] In large cities, it ranges from 9.7806[7] in Kuala Lumpur, Mexico City, and Singapore to 9.825 in Oslo and Helsinki." https://en.wikipedia.org/wiki/Gravity_of_Earth

Convection/thermals:
https://www.climate-policy-watcher.org/plate-tectonics/convection-and-the-earths-mantle-the.htmlAlso "Because the distribution of materials deep inside the Earth varies, its gravity field has hills and valleys"
OP NASA reference.
 
  • #20
StarHunter said:
"The acceleration g varies by about 1/2 of 1 percent with position on Earth’s surface, from about 9.78 meters per second per second at the Equator to approximately 9.83 meters per second per second at the poles." In OP Britannica reference.
Yes, that's a variation due to the change in altitude (the poles are about 13 miles closer to the Earth's center than the equator). You said you were talking about variations not due to change in altitude. (Strictly speaking, the equatorial value should also include the effects of the Earth's rotation; I'm not sure if the Britannica number does that.)

StarHunter said:
"Gravity on the Earth's surface varies by around 0.7%, from 9.7639 m/s2 on the Nevado Huascarán mountain in Peru to 9.8337 m/s2 at the surface of the Arctic Ocean.[6] In large cities, it ranges from 9.7806[7] in Kuala Lumpur, Mexico City, and Singapore to 9.825 in Oslo and Helsinki." https://en.wikipedia.org/wiki/Gravity_of_Earth
Again, these are variations due to changes in altitude and latitude (because the distance from the surface to the core varies with latitude), which you said is not what you were talking about.

StarHunter said:
Thanks, that makes it much clearer what you are referring to. I'm not sure if variation due to this is included in the variations the GRACE experiment measures.

StarHunter said:
Also "Because the distribution of materials deep inside the Earth varies, its gravity field has hills and valleys"
OP NASA reference.
Yes, the article does use the phrase "deep inside the Earth", but the rest of the article makes clear that by "deep" they mean "deep down in the crust" (for example, one person quoted says the GRACE data "can give us an idea of how much water is available deep in the Earth for irrigation and agriculture"--such water "deep in the Earth" still has to be somewhere in the crust, we can't extract water from the mantle or core), which, while "deep" on a human scale, is not very far inside the entire Earth.
 
  • #21
PeterDonis said:
Yes, that's a variation due to the change in altitude (the poles are about 13 miles closer to the Earth's center than the equator). You said you were talking about variations not due to change in altitude. (Strictly speaking, the equatorial value should also include the effects of the Earth's rotation; I'm not sure if the Britannica number does that.)
Yes, and when I was making my correction I was referring to the total measured deviation meaning that your value of 0.00001 m/s^2 is more likely to be accurate.
PeterDonis said:
Again, these are variations due to changes in altitude and latitude (because the distance from the surface to the core varies with latitude), which you said is not what you were talking about.
Correct
PeterDonis said:
Thanks, that makes it much clearer what you are referring to. I'm not sure if variation due to this is included in the variations the GRACE experiment measures.
I would think if it was a factor, then it would inevitably be measured but may have been nulled after running some math on the subject. Potentially figuring that it was a negligible variable.

PeterDonis said:
Yes, the article does use the phrase "deep inside the Earth", but the rest of the article makes clear that by "deep" they mean "deep down in the crust" (for example, one person quoted says the GRACE data "can give us an idea of how much water is available deep in the Earth for irrigation and agriculture"--such water "deep in the Earth" still has to be somewhere in the crust, we can't extract water from the mantle or core), which, while "deep" on a human scale, is not very far inside the entire Earth.
Good catch.

If it turns out 0.00001 m/s^2 is a more accurate measurement, then this makes a lot more sense to me.
 
  • #22
StarHunter said:
I would think if it was a factor, then it would inevitably be measured
From what I can gather, GRACE doesn't measure specific things that are causing the variations in ##g##; those have to be inferred. Such inferences would have to be based on other observations--for example, observing the hydrologic cycle directly in order to correlate variations in ##g## that GRACE measures with changes in water distribution, as the article describes. We don't have any way of directly observing the mantle so it might not be possible to correlate such variations with GRACE measurements.
 
  • #23
PeterDonis said:
From what I can gather, GRACE doesn't measure specific things that are causing the variations in ##g##; those have to be inferred. Such inferences would have to be based on other observations--for example, observing the hydrologic cycle directly in order to correlate variations in ##g## that GRACE measures with changes in water distribution, as the article describes. We don't have any way of directly observing the mantle so it might not be possible to correlate such variations with GRACE measurements.
Yes, I agree. Well said. And if thermal vectors were such a big factor, I would think we would see different deviation patterns and more generalized patterns. Although there are some larger area patterns they appear with altitude, mountain ranges, except for east USA where the Appalachian Mountains are. And I would expect an increase at volcanic sites or ranges. Maybe the material in the vectors is more homogeneous than I initially thought and are not pulling up more dense minerals/elements from closer to the core.
 

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1. What is free-fall gravity and how does it work?

Free-fall gravity is the force that pulls objects towards the center of the Earth. It is a fundamental force of nature that is caused by the mass of the Earth and the mass of the object. The greater the mass of an object, the stronger the force of gravity. This force is what keeps objects from floating off into space.

2. Why does free-fall gravity vary on different parts of the Earth?

The strength of free-fall gravity varies on different parts of the Earth due to a few factors. The first factor is the shape of the Earth, which is not perfectly spherical. This means that the distance from the center of the Earth to the surface is not the same everywhere. The second factor is the rotation of the Earth, which creates a centrifugal force that slightly counteracts the force of gravity. Lastly, the density of the Earth's crust and mantle can also affect the strength of free-fall gravity.

3. How do scientists measure the variations of free-fall gravity on Earth?

Scientists use a device called a gravimeter to measure the variations of free-fall gravity on Earth. This device measures the acceleration of gravity at a specific location and can detect even small changes in the strength of gravity. Scientists also use satellite data to map out the variations in free-fall gravity across the Earth's surface.

4. What are some factors that can cause changes in free-fall gravity over time?

There are a few factors that can cause changes in free-fall gravity over time. The first is tectonic activity, which can change the density and distribution of mass within the Earth's crust. Changes in the Earth's rotation and its orbit around the sun can also have an impact on free-fall gravity. Additionally, the melting of ice sheets and glaciers due to climate change can also cause small variations in free-fall gravity.

5. How does understanding variations in free-fall gravity on Earth benefit us?

Understanding variations in free-fall gravity on Earth can benefit us in many ways. It can help us better understand the structure and composition of the Earth's interior, as well as the processes that shape our planet. It can also aid in mapping out natural resources and predicting natural hazards such as earthquakes and volcanic eruptions. Additionally, understanding free-fall gravity can also have practical applications in fields such as geology, geophysics, and satellite navigation.

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