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A contrastive study on the influences of radial and three-dimensional satellite gravity gradiometry on the accuracy of the Earth's gravitational field recovery 下载免费PDF全文
The accuracy of the Earth’s gravitational field measured from the gravity field and steady-state ocean circulation explorer(GOCE),up to 250 degrees,influenced by the radial gravity gradient V zz and three-dimensional gravity gradient V ij from the satellite gravity gradiometry(SGG) are contrastively demonstrated based on the analytical error model and numerical simulation,respectively.Firstly,the new analytical error model of the cumulative geoid height,influenced by the radial gravity gradient V zz and three-dimensional gravity gradient V ij are established,respectively.In 250 degrees,the GOCE cumulative geoid height error measured by the radial gravity gradient V zz is about 2 1/2 times higher than that measured by the three-dimensional gravity gradient V ij.Secondly,the Earth’s gravitational field from GOCE completely up to 250 degrees is recovered using the radial gravity gradient V zz and three-dimensional gravity gradient V ij by numerical simulation,respectively.The study results show that when the measurement error of the gravity gradient is 3×10 12 /s 2,the cumulative geoid height errors using the radial gravity gradient V zz and three-dimensional gravity gradient V ij are 12.319 cm and 9.295 cm at 250 degrees,respectively.The accuracy of the cumulative geoid height using the three-dimensional gravity gradient V ij is improved by 30%-40% on average compared with that using the radial gravity gradient V zz in 250 degrees.Finally,by mutual verification of the analytical error model and numerical simulation,the orders of magnitude from the accuracies of the Earth’s gravitational field recovery make no substantial differences based on the radial and three-dimensional gravity gradients,respectively.Therefore,it is feasible to develop in advance a radial cold-atom interferometric gradiometer with a measurement accuracy of 10 13 /s 2-10 15 /s 2 for precisely producing the next-generation GOCE Follow-On Earth gravity field model with a high spatial resolution. 相似文献
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Accurate and rapid error estimation on global gravitational field from current GRACE and future GRACE Follow-On missions 总被引:10,自引:0,他引:10 下载免费PDF全文
Firstly, the new combined error model of cumulative geoid height
influenced by four error sources, including the inter-satellite range-rate
of an interferometric laser (K-band) ranging system, the orbital
position and velocity of a global positioning system (GPS) receiver
and non-conservative force of an accelerometer, is established from the
perspectives of the power spectrum principle in physics using the
semi-analytical approach. Secondly, the accuracy of the global
gravitational field is accurately and rapidly estimated based on the
combined error model; the cumulative geoid height error is 1.985×
10-1~m at degree 120 based on GRACE Level 1B measured
observation errors of the year 2007 published by the US Jet
Propulsion Laboratory (JPL), and the cumulative geoid height error is
5.825× 10^ - 2~m at degree 360 using GRACE Follow-On
orbital altitude 250~km and inter-satellite range 50 km. The
matching relationship of accuracy indexes from GRACE Follow-On key
payloads is brought forward, and the dependability of the combined error
model is validated. Finally, the feasibility of high-accuracy and
high-resolution global gravitational field estimation from GRACE
Follow-On is demonstrated based on different satellite orbital
altitudes. 相似文献
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