Abstract

During the past three decades, the Dead Sea (DS) water level has dropped at an average rate of ~1 m/year, resulting in the formation of thousands of sinkholes along its coastline that severely affect the economy and infrastructure of the region. The sinkholes are associated with gradual land subsidence, preceding their collapse by periods ranging from a few days to about five years. We present the results of over six years of systematic high temporal and spatial resolution interferometric synthetic aperture radar (InSAR) observations, incorporated with and refined by detailed Light Detection and Ranging (LiDAR) measurements. The combined data enable the utilization of interferometric pairs with a wide range of spatial baselines to detect minute precursory subsidence before the catastrophic collapse of the sinkholes and to map zones susceptible to future sinkhole formation. We present here four case studies that illustrate the timelines and effectiveness of our methodology as well as its limitations and complementary methodologies used for sinkhole monitoring and hazard assessment. Today, InSAR-derived subsidence maps have become fundamental for sinkhole early warning and mitigation along the DS coast in Israel and are incorporated in all sinkhole potential maps which are mandatory for the planning and licensing of new infrastructure.

Highlights

  • IntroductionCollapse sinkholes occur in a large number of geological environments around the globe e.g., [1,2,3]

  • Collapse sinkholes occur in a large number of geological environments around the globe e.g., [1,2,3].They generally form by the dissolution of subsurface soluble rocks, creating cavities that collapse when insufficiently supported [4,5,6]

  • The case studies presented in this study demonstrate the applicability of semi-automatic interferometric synthetic aperture radar (InSAR) monitoring to early warning, the updating of sinkhole susceptibility maps, and sinkhole hazard assessment and mitigation along the Dead Sea (DS) in Israel

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Summary

Introduction

Collapse sinkholes occur in a large number of geological environments around the globe e.g., [1,2,3]. They generally form by the dissolution of subsurface soluble rocks, creating cavities that collapse when insufficiently supported [4,5,6]. ~400 sinkholes in 2017 and peaked with ~700 new sinkholes in 2015 [14] Figure 2. This type of natural hazard affects the local agriculture, industry, tourism, infrastructure, and daily life in the region

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