Assesment of Coastal Subsidence and Inundation Risk due to Relative Sea Level Rise using MT-InSAR and Deep Learning Techniques over the Kerala Coast of India
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Abstract
Due to the increasing sea level rise and shoreline sinking, major coastal towns worldwide
face the risk of inundation from relative sea level changes [1]. Flooding has been a persis-
tent issue in Kerala, a southern Indian state, for the past few decades due to heavy rainfall
and the low elevation of the area. Large regions with a diversity of wildlife and people
can be found along Kerala’s 590 km of coastline which makes the region highly vulnerable
to inundation risk of relative sea level rise. In this context, we used a VV polarization to
examine Sentinel-1 data of European Space Agency (ESA) that was collected for tracking
subsidence along the descending track (Path 63 and 165). Using the Small Baseline Subset
(SBAS) based MT-InSAR technique, the entire Kerala is analyzed for Vertical Land Motion
(VLM) [2]. A total of 1443 interferograms were obtained by co-registering and processing
326 single-look complex images. The results show that the Kuttanad region of Alappuzha
and Cochin region of Ernakulam are having the maximum subsidence of >20 mm/year.
The tide gauge station on Cochin Willingdon Island shows a 1.97±mm/year relative sea
level trend. NASA’s Intergovernmental Panel on Climate Change (IPCC) AR6 assessment
has projected a future sea level shift of 0.71 meters by 2100, accounting for the socioeco-
nomic scenario SSP3-7.0. Utilizing the high spatial resolution of the Copernicus Digital
Elevation Model (DEM), the sea level projection data from the IPCC-AR6 report, and the
InSAR-derived VLM, the low-lying, rapidly subsiding zones that are susceptible to future
flood inundation due to relative sea level rise have been mapped for each of Kerala’s four-
teen districts. We have also incorporated a deep learning based U-net model to come up
with an automated risk map by considering the hazard, vulnerability and the susceptibility
of the region. A comparative analysis of the risk with and without considering Vertical
Land Motion was done to know the effect of subsidence on inundation. For the low level
scenario SSP 1-1.9, 4.53 to 14.82 % increase in the risk zone was observed when VLM was
also included. And for the high level scenario SSP 5-8.5, this percentage change was found
to be 4.71 to 9.94 %. This analysis will help policymakers take precautionary measures to
mitigate future disasters due to relative sea level rise.