Coastal subsidence detected by Synthetic Aperture Radar interferometry and its effects coupled with future sea-level rise: the case of the Sele Plain (Southern Italy)

The amount of coastal subsidence on the Sele River coastal plain has been
examined and measured with local vertical land movement data. The vertical
displacements, derived by satellite radar differential interferometry processing
(Ps-InSAR), show that the analysed coastal sector is characterised by a southeastward
decrease of vertical subsidence rates. These results have been coupled
with sea-level rise (SLR) scenarios, in order to identify the most critical areas. In
general, the subsidence mostly affects areas where alluvial deposits are thicker,
the back-dune areas and the Sele River mouth, all late Holocene in age. Five local
SLR scenarios allow identifying zones in the plain potentially prone to inundation
and the shoreline retreat for the years 2065 and 2100. For these dates, 2.2%
and 7.06% of the investigated area will have a topography lower than the estimated
future sea level. Moreover, results show that the extent of the areas potentially
exposed to inundation and erosion increases moving from south to north.

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