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The discrepancy is small, generally a few tens of centimetres or less, but it can be determined by a comparison of satellite radar measurements of sea-surface shape with the shape calculated from the very best estimates of the Earth's total gravity field.
Gray and thick solid lines are observed gravity, gobs(t), and estimated total gravity, gcal(t), respectively.
The value ε is an infinitesimal number (ε ≤ 10−6) to avoid some singularities; it represents at the maximum only 1 μGal in the total gravity values.
(b) Thin, gray and thick lines are estimated drift component, gd(t), observed gravity, gobs(t) and estimated total gravity, gcal(t), respectively.
Lower thick and gray lines are total gravity change due to soil moisture with and without the building effect, (Eq. (28)) and gw(t) (Eq. (17)), respectively.
The recovered gravity field from satellite data appears to contribute mainly to medium and long wavelength parts of total gravity field spectrum.
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As a result, the total specific gravity became slightly smaller than 1.
As a result, the total specific gravity became slightly smaller than 1, as shown in Table 2.
By definition, P i,j and P i = ∑ i m ∑ j=0 n P i,j are nodal and total accumulative gravity loads acting on level i, respectively.
Both baryonic and dark matter contribute to and are affected by the total self-gravity of the system.
The thick line in Fig. 6(b) shows the predicted total change in gravity, Although gcal(t) qualitatively reproduces gravity increases during precipitation events, the amount of the increase for the calculated gravity is about twice that of the observed gravity (gray line), as seen in April 2009, July 2010 and September 2010.
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