Abstract
As part of the work of the SEASAT user research group of Europe altimeter data of SEASAT-1, preprocessed by Jet Propulsion Laboratories, have been used to derive a high-precision geoid as well as gravity anomalies für the North Sea Area. The altimeter data have been corrected first for tidal effects; the tidal signal was computed at the Institute of Oceanographic Science, Bidston, using a high precision tidal model for the North Sea.
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Reference
Brennecke,J. and D.Lelgemann (1983) Geoid and Gravity Anomalies in the North Sea Area derived from SEASAT Altimeter Data. Manuscripta Geodaetica, Vol.8 (1983), p.3o1–32o.
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© 1984 Springer Science+Business Media Dordrecht
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Brennecke, J., Lelgemann, D. (1984). Geoid and Gravity Anomalies in the North Sea Area Derived from SEASAT-Altimeter Data. In: Seeber, G., Apel, J.R. (eds) Geodetic Features of the Ocean Surface and their Implications. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1673-4_9
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DOI: https://doi.org/10.1007/978-94-017-1673-4_9
Publisher Name: Springer, Dordrecht
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