Abstract
The Gravity and Ocean Circulation Experiment - GOCE satellite mission measure the Earth gravity field with unprecedented accuracy leading to substantial improvements in the modelling of the ocean circulation and transport. In this study of the performance of GOCE, a newer gravity model has been combined with the DTU10MSS mean sea surface model to construct a global mean dynamic topography model named DTU10MDT. The results of analyses clearly demonstrated the value of the GOCE mission. Both the resolution and the estimation of the surface currents have been improved significantly compared to results obtained using pre-GOCE gravity field models. The results of this study show that geostrophic surface currents associated with the mean circulation have been further improved and that currents having speeds down to 5 cm/s have been recovered.
Original language | English |
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Title of host publication | Proceedings of ESA Living Planet Symposium |
Publisher | European Space Agency |
Publication date | 2013 |
Publication status | Published - 2013 |
Event | ESA Living Planet Symposium — 2013 - Edinburgh, United Kingdom Duration: 9 Sept 2013 → 13 Sept 2013 |
Conference
Conference | ESA Living Planet Symposium — 2013 |
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Country/Territory | United Kingdom |
City | Edinburgh |
Period | 09/09/2013 → 13/09/2013 |