Abstract

A methodology for the remotely sensed monitoring, measurement and quantification of littoral zone platform downwearing has been developed and is demonstrated, using Persistent Scatterer Interferometric Synthetic Aperture Radar data and analysis. The research area is a 30 km section of coast in East Sussex, UK. This area combines a range of coastal environments and is characterised by the exposure of chalk along the cliffs and coastal platform. Persistent Scatterer Interferometry (PSI) has been employed, using 3.5 years of Sentinel-1 SAR data. The results demonstrate an average ground level change of −0.36 mm a−1 across the research area, caused by platform downwearing. Protected sections of coast are downwearing at an average of −0.33 mm a−1 compared to unprotected sections, which are downwearing more rapidly at an average rate of −1.10 mm a−1. The material properties of the chalk formations in the platform were considered, and in unprotected areas the weakest chalk types eroded at higher rates (−0.66 mm a−1) than the more resistant formations (−0.53 mm a−1). At a local scale, results were achieved in three studies to demonstrate variations between urban and rural environments. Individual persistent scatterer point values provided a near-continuous sequence of measurements, which allowed the effects of processes to be evaluated. The results of this investigation show an effective way of retrospective and ongoing monitoring of platform downwearing, erosion and other littoral zone processes, at regional, local and point-specific scales.

Highlights

  • 10% of the world’s population lives in coastal zones [1], and, as a result of weather patterns, climate change, rising sea levels and anthropological activities, many coastal communities are at risk of the effects of erosion and flooding

  • This study focused on the chalk cliffs and platform of East Sussex because chalk is considered a very weak to weak rock which is susceptible to rapid erosion and weathering [7] and is an ideal target for monitoring coastal erosion and processes that are quantifiable over relatively short time periods and can be used as analogues for other coastal environments

  • The results are presented as time series plots, with the period of time over which the analysis was performed on the horizontal axis and the amount of ground movement in the line of sight (LoS) towards the satellite on the vertical axis

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Summary

Introduction

10% of the world’s population lives in coastal zones [1], and, as a result of weather patterns, climate change, rising sea levels and anthropological activities, many coastal communities are at risk of the effects of erosion and flooding. This study focused on the chalk cliffs and platform of East Sussex because chalk is considered a very weak to weak rock (of a strength between 1–25 MPa) which is susceptible to rapid erosion and weathering [7] and is an ideal target for monitoring coastal erosion and processes that are quantifiable over relatively short time periods and can be used as analogues for other coastal environments This particular section of chalk coast has been the subject of multiple studies of shore platform erosion over many years, and forms the most suitable site for this research

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