When using the ocean dynamics correction, the results
are stable in Senetosa, with a homogenisation of the bias
estimates as the mean biases dispersion decreases from
1 cm to 0.3 cm. A general decrease of about 0.7 cm, which
is a little beyond the standard error (0.4 cm), is observed in
the bias estimates in Senetosa when using the ocean
dynamics correction, whereas, the bias increases by about
1 cm in Ajaccio. This is very coherent with what was
observed in the case of the Jason-2 mission in the previous
section and confirms that the estimation of the tide correction
at the Ajaccio tide gauge is dubious, probably because
of the location of the instrument.