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Most intriguing is the controversial trend between the gravity changes and the vertical deformation.
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A grid search algorithm was applied to determine the saturated permeability (K s ) and diffusivity (D s ) of the soil and the admittance between the gravity change and the water content at each site (see Additional file 1 for more details).
Some strike-slip faults from geology data in the north-east area at KGF are also correlated to the gravity changes distribution between 1999 and 2008.
The gravity changes are larger in the high permeability zone.
The gravity changes in this period is the largest compared to the gravity changes average rate of two previous periods.
The gravity changes from the repeat gravity measurement (RGM) directly illustrate the mass variation in the subsurface.
The model can reproduce the gravity change with a permeability range between those suggested by laboratory experiments and numerical simulations of slow earthquakes.
Then, the misfit between the new resulting gravity and the reference one is computed, leading to the gravity change of geothermal origin.
The gravity change of the M rr component is responsible mostly for the positive gravity at P2, while the one of M θθ − M φφ is for the negative gravity change at P1 and P3.
We discuss a temporal coincidence between the residual gravity change and the LSSEs and try to interpret it with a simple poroelastic model ("Discussion" section).
Through correlation analysis, we find a moderate positive correlation between the amplitudes of the annual gravity changes and the shallow background seismicity rates at the worldwide subduction zones excluding the source areas of large earthquakes.
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