Abstract. In the context of the ESA Climate Change Initiative project, we are engaged
in a regional reprocessing of high-resolution (20 Hz) altimetry data of the
classical missions in a number of the world's coastal zones. It is done using
the ALES (Adaptive Leading Edge Subwaveform) retracker combined with the
X-TRACK system dedicated to improve geophysical corrections at the coast.
Using the Jason-1 and Jason-2 satellite data, high-resolution, along-track sea
level time series have been generated, and coastal sea level trends have been
computed over a 14-year time span (from July 2002 to June 2016). In this
paper, we focus on a particular coastal site where the Jason track crosses
land, Senetosa, located south of Corsica in the Mediterranean Sea, for two
reasons: (1) the rate of sea level rise estimated in this project increases
significantly in the last 4–5 km to the coast compared to what is observed
further offshore, and (2) Senetosa is the calibration site for the
TOPEX/Poseidon and Jason altimetry missions, which are equipped for that purpose with
in situ instrumentation, in particular tide gauges and a Global Navigation Satellite System (GNSS) antenna. A
careful examination of all the potential errors that could explain the
increased rate of sea level rise close to the coast (e.g., spurious trends
in the geophysical corrections, imperfect inter-mission bias estimate,
decrease of valid data close to the coast and errors in waveform retracking)
has been carried out, but none of these effects appear able to explain the
trend increase. We further explored the possibility that it results from real
physical processes. Change in wave conditions was investigated, but wave setup was excluded as a potential contributor because the magnitude was too low
and too localized in the immediate vicinity of the shoreline. A preliminary
model-based investigation about the contribution of coastal currents
indicates that it could be a plausible explanation of the observed change in
sea level trend close to the coast.