Abstract

The use of satellite SAR interferometric methods has significantly improved the monitoring of ground movements over the last decades, thus opening new possibilities for a more accurate interpretation of land subsidence and its driving mechanisms. TerraSAR-X has been extensively used to study land subsidence in the Venice Lagoon, Italy, with the aim of quantifying the natural and anthropogenic causes. In this paper, we review and update the main results achieved by three research projects supported by DLR AOs (German Aerospace Center Announcement of Opportunity) and conducted to test the capability of TerraSAR-X PSI (Persistent Scatterer Interferometry) to detect ground movements in the complex physiographic setting of the Venice transitional coastal environment. The investigations have been focused on the historical center of Venice, the lagoon inlets where the MoSE is under construction, salt marshes, and newly built-up areas in the littoral. PSI on stacks of stripmap TerraSAR-X images covering short- to long-time periods (i.e., the years 2008–2009, 2008–2011 and 2008–2013) has proven particularly effective to measure land subsidence in the Venice coastland. The very high spatial resolution (3 m) and the short repeat time interval (11 days) of the TerraSAR-X acquisitions make it possible to investigate ground movements with a detail unavailable in the past. The interferometric products, properly calibrated, allowed for a millimetric vertical accuracy of the land movements at both the regional and local scales, even for short-term analyses, i.e., spanning one year only. The new picture of the land movement resulted from processing TerraSAR-X images has significantly contributed to update the knowledge on the subsidence process at the Venice coast.

Highlights

  • The city of Venice and its surrounding lagoon is presently one of the sites most sensitive to land subsidence worldwide

  • We review and update the main results achieved by three research projects supported by DLR AOs (German Aerospace Center Announcement of Opportunity) and conducted to test the capability of TerraSAR-X PSI (Persistent Scatterer Interferometry) to detect ground movements in the complex physiographic setting of the Venice transitional coastal environment

  • Land subsidence and climate change effects concurred to a relative sea level rise (RSLR) in Venice equal to 26 cm [1], a situation that is expected to get dramatically worst if we consider the 53 cm sea level rise projected by the Intergovernmental Panel on Climate Change (IPCC) in 2100 according to the A1B scenario, which accounts for a future energy system balanced between fossil and non-fossil sources [2]

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Summary

Introduction

The city of Venice and its surrounding lagoon is presently one of the sites most sensitive to land subsidence worldwide. The subsidence monitoring network of the Venice coastland increased from a few hundreds of benchmarks measured by leveling [3] to a few hundred thousand reflectors detected by SAR-based interferometry using ERS and ENVISAT satellites [4]. Concerning the Venice Lagoon, three projects have been carried out over the last decade under the umbrella of the DLR AOs: LAN0242 “Monitoring land subsidence in Venice”; COA0612 “Assessing vertical movements of natural tidal landforms and anthropogenic structures at the Venice Lagoon inlets”; and COA1800 “Ground surface dynamics in the Venice Lagoon: five years of monitoring of natural tidal landforms and anthropogenic structures by TerraSAR-X” These projects have allowed testing the effectiveness of TerraSAR-X in quantifying land subsidence in the Venice coastland with the aim of improving the knowledge on natural and anthropogenic causes. The goal of this paper is to provide a review of the main results and advancements in the knowledge of land subsidence at the Venice coastland achieved by TerraSAR-X PSI over the last decade, updating the main outcomes obtained in the past years with the analyses recently carried out over the six-year period between 2008 and 2013

TerraSAR-X Image Processing and Output Calibration
Ground Displacements at the Regional Scale
Ground Displacement at the Local-Scale
Induced Ground Movements in the Historical Center of Venice
Salt Marshes Ground Dynamics
Findings
The MoSE Constructions at the Lagoon Inlets
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