2015Acta Scientiarum Naturalium Universitatis SunyatseniRequires access

Progress in satellite gravity recovery from implemented CHAMP, GRACE and GOCE and future GRACE Follow-On missions

Zheng, Wei, Xu, Houze

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Abstract

Firstly,the Earth’s gravitational field from the past Challenging Minisatellite Payload(CHAMP) mission is determined using the energy conservation principle,the combined error model of the cumulative geoid height influenced by three instrument errors from the current Gravity Recovery and Climate Experiment(GRACE) and future GRACE Follow-On missions is established based on the semi-analytical method,and the Earth’s gravitational field from the executed Gravity Field and Steady-State Ocean Circulation Explorer(GOCE) mission is recovered by the space-time-wise approach.Secondly,the cumulative geoid height errors are 1.727 × 10-1 m,1.839 × 10 -1 m and 9.025 × 10-2 m at degrees 70,120 and 250 from the implemented three-stage satellite gravity missions consisting of CHAMP,GRACE and GOCE,which preferably accord with those from the existing earth gravity field models involving EIGEN-CHAMP03 S,EIGEN-GRACE02 S and GOCONSGCF2DIRR1.The cumulative geoid height error is 6.847 × 10-2 m at degree 250 from the future GRACE Follow-On mission.Finally,the complementarity among the four-stage satellite gravity missions including CHAMP,GRACE,GOCE and GRACE Follow-On is demonstrated contrastively.

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What this paper is about

Firstly,the Earth’s gravitational field from the past Challenging Minisatellite Payload(CHAMP) mission is determined using the energy conservation principle,the combined error model of the cumulative geoid height influenced by three instrument errors from the current Gravity Recovery and Climate Experiment(GRACE) and future GRACE Follow-On missions is established based on the semi-analytical method,and the Earth’s gravitational field from the executed Gravity Field and Steady-State Ocean Circulation Explorer(GOCE) mission is recovered by the space-time-wise approach.Secondly,the cumulative geoid height errors are 1.727 × 10-1 m,1.839 × 10 -1 m and 9.025 × 10-2 m at degrees 70,120 and 250 from the implemented three-stage satellite gravity missions consisting of CHAMP,GRACE and GOCE,which preferably accord with those from the existing earth gravity field models involving EIGEN-CHAMP03 S,EIGEN-GRACE02 S and GOCONSGCF2DIRR1.The cumulative geoid height error is 6.847 × 10-2 m at degree 250 from the future GRACE Follow-On mission.Finally,the complementarity among the four-stage satellite gravity missions including CHAMP,GRACE,GOCE and GRACE Follow-On is demonstrated contrastively.

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Available abstract

Firstly,the Earth’s gravitational field from the past Challenging Minisatellite Payload(CHAMP) mission is determined using the energy conservation principle,the combined error model of the cumulative geoid height influenced by three instrument errors from the current Gravity Recovery and Climate Experiment(GRACE) and future GRACE Follow-On missions is established based on the semi-analytical method,and the Earth’s gravitational field from the executed Gravity Field and Steady-State Ocean Circulation Explorer(GOCE) mission is recovered by the space-time-wise approach.Secondly,the cumulative geoid height errors are 1.727 × 10-1 m,1.839 × 10 -1 m and 9.025 × 10-2 m at degrees 70,120 and 250 from the implemented three-stage satellite gravity missions consisting of CHAMP,GRACE and GOCE,which preferably accord with those from the existing earth gravity field models involving EIGEN-CHAMP03 S,EIGEN-GRACE02 S and GOCONSGCF2DIRR1.The cumulative geoid height error is 6.847 × 10-2 m at degree 250 from the future GRACE Follow-On mission.Finally,the complementarity among the four-stage satellite gravity missions including CHAMP,GRACE,GOCE and GRACE Follow-On is demonstrated contrastively.

Key concepts: Gravitational field, Geoid, Gravity of Earth, Geodesy, Satellite, Geodetic datum, Geology, Geopotential

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Progress in satellite gravity recovery from implemented CHAMP, GRACE and GOCE and future GRACE Follow-On missions — Research Paper | ScholarLens