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Variations in distance caused by gravity difference on earth produce data points for the gravity map.
First of all, waste ion exchange resins were separated into cationic and anionic resins by a specific gravity difference in the fluidized bed.
A tidal prediction shows that the gravity difference between Strasbourg and Soultz (40-km distance) leads to a very small residual tidal signal with a standard deviation of 0.45 μGal.
The gravity difference,, seems to be positive in summer (June August) and negative in winter and spring (February May), implying the existence of an annual gravity signal in gobs(t).
Moreover, the gravity difference is within 1 µgal for the changes in a (Fig. 13(c)) and b (Fig. 14(c)), and is exactly zero for changes of P0 (Fig. 15(c)).
Additionally, there is no need of height correction for the gravity difference at the crossover point because of the insensitivity of gravity anomaly to height difference around the mean flight altitude.
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Subtle gravity differences can also provide information about the structure of earth's interior, including the tectonic processes that continue to reshape the surface and move continents.
b Gravity differences at crossover points.
Figure 3b shows the gravity differences after the adjustment.
c Gravity differences (gravity values in 2013 relative to those in 1994).
Most of the gravity differences in Fig. 9 fall between ±10 mGal.
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Justyna Jupowicz-Kozak
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