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Quote from: Janus on 08/05/2018 18:10:11No, it doesn't. GRACE is measuring the local field strength at a fixed altitude. From this, you could calculate the field strength at any other fixed altitude (say, Mean Sea Level). This means that the map does not represent the value of g at the actual physical surface, But the difference in measured g at the same altitude for different parts of the globe. So are you saying that when GRACE takes these measurements over the top of the mountain (or valley), that gravity is not reducing by the inverse square law within the distance between the mountain top (or valley) and GRACE's position of altitude?That gravity is somehow weaker at the mountain top than GRACE actually reads, and stronger in the valley than GRACE actually reads?
No, it doesn't. GRACE is measuring the local field strength at a fixed altitude. From this, you could calculate the field strength at any other fixed altitude (say, Mean Sea Level). This means that the map does not represent the value of g at the actual physical surface, But the difference in measured g at the same altitude for different parts of the globe.
Since sea level automatically follows the surface of equipotential, clocks at MSL would be subject to the same equipotential, and would run at the same rate. So the reason why sea level settles where it does, and why clocks at this level all run at an equal rate is one and the same.
I am saying that GRACE is not measuring the strength of gravity at the mountain top or valley floor, but the strength of gravity at the altitude of where GRACE is and to determine the actual local strength of gravity at the Mountain top or valley floor, you do have to take into account fact that gravity falls off by the square of distance and that the valley floor is closer to the center of the Earth than the Mountain top.
Quote from: Janus on 08/05/2018 19:02:45I am saying that GRACE is not measuring the strength of gravity at the mountain top or valley floor, but the strength of gravity at the altitude of where GRACE is and to determine the actual local strength of gravity at the Mountain top or valley floor, you do have to take into account fact that gravity falls off by the square of distance and that the valley floor is closer to the center of the Earth than the Mountain top.Ok - I will take what you say on board - but if I imagine how GRACE manages their data it kind of goes like this:Got a gravity reading.Where are we?What distance to surface?Use of square (? terminology check "as opposed to inversed square") places gravity strength at top of mountain as ? Places gravity at bottom of valley as?But perhaps my imagination doesn't serve me well, and I am mistaken?
GRACE Consists of two satellites following each other closely in orbit. The gravitational variations are mapped by carefully measuring how the distance between the two satellites change as they pass over different points of the globe. This tells the satellites how much the Earth's gravitational field varies. And this variation is what the map represents. It is not a map of how local gravity changes at local ground level. You could work this out from the Grace data and the topological data, But Grace doesn't, because that's not what the research is about, but rather the general "shape" of the Earth's gravity field. It is about how mass distribution caused by a number a factors (crustal thickness and density for example) effects the measurement of g from point to point on the Earth, Without worrying about the local changes due to local altitude. In the case of this study, those variations in " on the spot" measurements in g caused by differences in altitude at ground level is noise to be ignored in order to get to the more interesting data underneath.
The only way to measure g at a point, is to take a gravimeter there.