Abstract
A numerical study has been conducted in order to estimate how a gravity field model obtained from GOCE data can be improved in the range of low degrees by addition of GRACE data. The GRACE data are simulated as inter-satellite accelerations. Different types of noise in the inter-satellite accelerations are considered, including white noise. The gravity field model is represented as a series of spherical harmonics; the Stokes coefficients are computed by a least-squares adjustment. It is shown that the incorporation of GRACE data may improve a GOCE-based gravity field model up to degree 120 or even higher depending on the type of noise in the inter-satellite accelerations. Moreover, the joint model at lower degrees may show a significantly higher quality that either a stand-alone GOCE-based or a stand-alone GRACE-based model. It is important, however, that proper covariance matrices of the involved data sets are used in the joint data processing.
Original language | English |
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Title of host publication | Dynamic Planet |
Subtitle of host publication | Monitoring and Understanding a Dynamic Planet with Geodetic and Oceanographic Tools - lAG Symposium |
Pages | 403-409 |
Number of pages | 7 |
Volume | 130 |
DOIs | |
Publication status | Published - 1 Dec 2007 |
Externally published | Yes |
Event | IAG Symposium on Dynamic Planet: Monitoring and Understanding a Dynamic Planet with Geodetic and Oceanographic Tools - Cairns, QLD, Australia Duration: 22 Aug 2005 → 26 Aug 2005 |
Conference
Conference | IAG Symposium on Dynamic Planet: Monitoring and Understanding a Dynamic Planet with Geodetic and Oceanographic Tools |
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Country/Territory | Australia |
City | Cairns, QLD |
Period | 22/08/05 → 26/08/05 |
Keywords
- Earth's gravity field
- GOCE
- GRACE
- Gravity gradiometry
- Inter-satellite accelerations
ASJC Scopus subject areas
- Computers in Earth Sciences
- Geophysics