Abstract
In altimetric measurements we observe the height of a satellite on the actual sea surface ( Hobs ). This quantity (see Fig. 1) can be modelled as:
where h is the satellite’s height referred to the ellipsoid, N is the geoid, ζ the sea surface topography, splitted into stationary component ( ζo ) and time dependent component ( ζ✝ ) and v is the noise.
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References
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© 1991 Springer-Verlag New York Inc.
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Barzaghi, R., Brovelli, M., Sansó, F. (1991). Altimetry Rank Deficiency in Crossover Adjustment. In: Rapp, R.H., Sansò, F. (eds) Determination of the Geoid. International Association of Geodesy Symposia, vol 106. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-3104-2_13
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DOI: https://doi.org/10.1007/978-1-4612-3104-2_13
Publisher Name: Springer, New York, NY
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