A GWR superconducting gravimeter of the new generation (OSG-60) has been installed in July 2010 in sub-humid West Africa, at the Djougou station in Benin. This station is part of the AMMA-CATCH Observatory for environmental research. We present the first results in terms of instrumental drift as well as the calibration results using FG5 absolute gravity measurements. We show that geophysical contributions due to hydrological load can bias the initial drift estimate. The noise level is compared to the Strasbourg SG as well as to the reference New Low Noise Model (NLNM) used in seismology. We also investigate the gravity response to atmospheric pressure changes and show that, because of the presence of large thermal tides, the gravity response to mass changes in the atmosphere is more complex than in the simple case of a constant barometric admittance.

Preliminary results from the superconducting gravimeter SG-060 installed in West Africa (Djougou, Benin) / Hinderer, J.; Rosat, S.; Calvo, M.; Boy, J. P.; Hector, B.; Riccardi, Umberto; Seguis, L.. - STAMPA. - 139:(2014), pp. 413-419. [10.1007/978-3-642-37222-3_55]

Preliminary results from the superconducting gravimeter SG-060 installed in West Africa (Djougou, Benin)

RICCARDI, UMBERTO;
2014

Abstract

A GWR superconducting gravimeter of the new generation (OSG-60) has been installed in July 2010 in sub-humid West Africa, at the Djougou station in Benin. This station is part of the AMMA-CATCH Observatory for environmental research. We present the first results in terms of instrumental drift as well as the calibration results using FG5 absolute gravity measurements. We show that geophysical contributions due to hydrological load can bias the initial drift estimate. The noise level is compared to the Strasbourg SG as well as to the reference New Low Noise Model (NLNM) used in seismology. We also investigate the gravity response to atmospheric pressure changes and show that, because of the presence of large thermal tides, the gravity response to mass changes in the atmosphere is more complex than in the simple case of a constant barometric admittance.
2014
9783642372216
Preliminary results from the superconducting gravimeter SG-060 installed in West Africa (Djougou, Benin) / Hinderer, J.; Rosat, S.; Calvo, M.; Boy, J. P.; Hector, B.; Riccardi, Umberto; Seguis, L.. - STAMPA. - 139:(2014), pp. 413-419. [10.1007/978-3-642-37222-3_55]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11588/502389
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