2016
DOI: 10.1007/s11200-015-0634-2
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Abstract: An airborne gravity campaign was carried out at the Dome-C survey area in East Antarctica between the 17th and 22nd of January 2013, in order to provide data for an experiment to validate GOCE satellite gravity gradients. After typical filtering for airborne gravity data, the cross-over error statistics for the few crossing points are 11.3 mGal r.m.s., corresponding to an r.m.s. line error of 8.0 mGal. This number is relatively large due to the rough flight conditions, short lines and field handling procedures… Show more

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Cited by 3 publications
(1 citation statement)
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“…This method was used to generate the gravitational gradients at satellite altitude from the ground gravity data to validate the SGG data. The airborne gravity data of the Antarctic region were applied to validate the GOCE gravity gradiometry data in Yildiz et al (Yildiz, 2012;Yildiz et al, 2016). They concluded that the differences between the calculated gravitational gradients from the LSC upward continuation method and the GOCE gravitational gradient observations were 9.9 mE, 11.5 mE, 11.6 mE, and 10.4 mE in the high-precision components Vxx, Vyy, Vzz, and Vxz, respectively.…”
Section: Introductionmentioning
confidence: 99%
“…This method was used to generate the gravitational gradients at satellite altitude from the ground gravity data to validate the SGG data. The airborne gravity data of the Antarctic region were applied to validate the GOCE gravity gradiometry data in Yildiz et al (Yildiz, 2012;Yildiz et al, 2016). They concluded that the differences between the calculated gravitational gradients from the LSC upward continuation method and the GOCE gravitational gradient observations were 9.9 mE, 11.5 mE, 11.6 mE, and 10.4 mE in the high-precision components Vxx, Vyy, Vzz, and Vxz, respectively.…”
Section: Introductionmentioning
confidence: 99%