Table 4
Jason-2 mean bias estimates on the nominal orbit in Senetosa and in Ajaccio, using the regional method and considering or not the ocean dynamics
correction. The number of cycles corresponds to the altimeter data between cycles 1 and 93 for which it was possible to estimate the bias as some lowquality
measurements were eliminated. In the case of Ajaccio, the number of cycles is dramatically reduced due to the gap of one year and a half in the tide
gauge time series.