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Preprocessing of gravity gradients at the GOCE high-level processing facility

Authors :
M. Veicherts
Pieter Visser
Sietse M. Rispens
Ernst Schrama
R. Koop
Carl Christian Tscherning
Thomas Gruber
Johannes Bouman
Source :
Journal of Geodesy, 83 (7)
Publisher :
Springer Nature

Abstract

One of the products derived from the gravity field and steady-state ocean circulation explorer (GOCE) observations are the gravity gradients. These gravity gradients are provided in the gradiometer reference frame (GRF) and are calibrated in-flight using satellite shaking and star sensor data. To use these gravity gradients for application in Earth scienes and gravity field analysis, additional preprocessing needs to be done, including corrections for temporal gravity field signals to isolate the static gravity field part, screening for outliers, calibration by comparison with existing external gravity field information and error assessment. The temporal gravity gradient corrections consist of tidal and nontidal corrections. These are all generally below the gravity gradient error level, which is predicted to show a 1/f behaviour for low frequencies. In the outlier detection, the 1/f error is compensated for by subtracting a local median from the data, while the data error is assessed using the median absolute deviation. The local median acts as a high-pass filter and it is robust as is the median absolute deviation. Three different methods have been implemented for the calibration of the gravity gradients. All three methods use a high-pass filter to compensate for the 1/f gravity gradient error. The baseline method uses state-of-the-art global gravity field models and the most accurate results are obtained if star sensor misalignments are estimated along with the calibration parameters. A second calibration method uses GOCE GPS data to estimate a low-degree gravity field model as well as gravity gradient scale factors. Both methods allow to estimate gravity gradient scale factors down to the 10?3 level. The third calibration method uses high accurate terrestrial gravity data in selected regions to validate the gravity gradient scale factors, focussing on the measurement band. Gravity gradient scale factors may be estimated down to the 10?2 level with this method.

Details

Language :
English
ISSN :
09497714 and 14321394
Volume :
83
Issue :
7
Database :
OpenAIRE
Journal :
Journal of Geodesy
Accession number :
edsair.doi.dedup.....72cd57799bf8b8940242118e668950f6
Full Text :
https://doi.org/10.1007/s00190-008-0279-9