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Data from "Direct measurement of subsurface mass change using the variable baseline gravity gradient method"

Summary

Data from Kennedy, J., Ferré, T.P.A., Güntner, A., Abe, M., and Creutzfeldt, B., 2014, Direct measurement of subsurface mass change using the variable baseline gravity gradient method: Geophysical Research Letters, v. 41, no. 8, p. 2827–2834.doi: 10.1002/2014GL059673 Collected using two iGrav superconducting gravimeters located about 15 m and 30 m from the edge of a 83,000 m^2 infiltration basin. Data are in tsoft format, with the channels: iGrav6 residual: [3]*(-914.6)-[6]-[4]*(-3.6902) iGrav4 residual: [1]*(-932.54)-[5]-[2]*(-3.263) Local tide model - BTG: Local tide model fitted using BAYTAP-G and data from the respective gravimeter. Residual - sc: Stage-corrected residual, with the gravitational attraction of water ponded [...]

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GL059163.zip 19.41 MB
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