Adamu Abubakar Please give specifics of the data sources you want to use. Clear enough so that anyone can understand and use the source. Please read Article Gravity surveys using a mobile atom interferometer (They are not the best, but you should know what that kind of instrument can do) Please read Article Status
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Accelerometers and gradiometers get better at higher frequencies, use the Internet to multiply capabilities many fold https://www.researchgate.net/project/Solar-System-Gravimetry-and-Gravitational-Engineering These “updates” are just things I think are important to remember, and what I can find time and energy to write down. If you see something you disagree with, write me or make a comment. I got a
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https://www.researchgate.net/project/Solar-System-Gravimetry-and-Gravitational-Engineering/ Calibrating all gravitational sensors into a single imaging array: I was thinking about this some more. The gravitational potential from the sun and moon changes significantly during the year and over the course of the day. And the absolute values (for the usual network few hundred samples per second and slower) change slowly. Your
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https://www.researchgate.net/publication/359389325_ON_THE_NORMAL_HEIGHT_DIFFERENCES_DETERMINATION_FROM_GEOPOTENTIAL_DIFFERENCES/comments Using real time comparisons via electromagnetic signals gets more complicated. Trying to use high speed storage of the signals gets memory intensive and expensive. As much of the data is nearly the same. The reason I used the vector tidal gravity signals for calibration and standardization is that each location can compare to
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Low Cost, Time-of-Flight Gravimeter Arrays https://hackaday.io/project/164550-low-cost-time-of-flight-gravimeter-arrays More information posted at ResearchGate on 3 axis gravimeters RichardCollins • 07/19/2022 at 17:15 • 0 comments My main “job” is the Internet Foundation, so I am constantly monitoring global issues, methods and activities on the Internet. But I have a heart for research groups and gravitational noise detector
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Vector sun moon tidal signal from gravimeter arrays is pure Newtonian GMm/r2. Sample at Msps Gsps for G variations by frequency at continuous global Big G stations to constrain sun moon earth masses, omegaE, JPL ephemeris, gravitational time dilation. https://hackaday.io/project/164550/gallery#21f5826751cf7b199a02263bd201e9bb You might be interested in my project on ResearchGate. I added an update today about
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The Planck Temperature – Absolute Hot: What is the hottest temperature possible https://www.youtube.com/watch?v=ofzlBP6_5iw If you had a $Thank button, I would have sent you a donation to encourage you to keep going and work harder. You have the right kind of curiosity, but you need to keep digging and read harder papers. Tone down “strange”
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This intro added 10 Jul 2022 in update to “Solar System Gravimetry and Gravitational Engineering ” Comment on “MegaAmpere to MegaGauss” – Using laser fluctuations to measure gravitational potential turbulence To generate intense fields to control the motion of matter. To emulate gravitational acceleration so precisely there is almost no error in position or other
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For more than 50 years I have been trying to understand the gravitational potential. I used it for orbit determinations when I worked at my first job at the CIA, then later worked on a NASA project to determine the geopotential itself using satellite orbits and measurements to solve for the shape and properties of
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Everyone, I am including this as an update to this project because the routine laboratory and wide area measurement of the speed of the gravitational potential is critical to all the groups working together. You HAVE to be able to measure the signals at high enough sampling rates to get good correlations and comparisons. For
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