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Natural versus anthropogenic subsidence of Venice : investigation of the present occurrence by Persistent scatterer interferometry P. Teatini a,b , L. Tosi b , T. Strozzi c. a Dept of Civil, Environmental and Architectural Engineering, University of Padova , Italy
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Natural versus anthropogenic subsidence of Venice: investigation of the present occurrence by Persistent scatterer interferometry P. Teatini a,b, L. Tosi b,T. Strozzi c aDept of Civil, Environmental and Architectural Engineering, University of Padova, Italy b Institute of Marine Sciences, National Research Council, Venice, Italy c Gamma Remote Sensing, Gumligen, Switzerland Sinking coastal cities Press conference, Monday, 28 April, 14:00
INTRODUCTION Contributions to the RLS (relative land subsidence) at Venice VENICE Location of the Venice Lagoon Consequences of RLS at Venice
PRESENT LAND SUBSICENCE OF VENICE Average displacement rates (mm/yr) obtained by Persistent Scatterer Interferometry at Venice ENV 2003-2010: 1.0 0.7 mm/yr ERS 1992-2002: 0.8 0.7 mm/yr TSX 2008: 1.0 1.6 mm/yr CSK 2008-2011: 1.1 1.0 mm/yr
SPLITTING NATURAL AND ANTHOPOGENIC SUBSIDENCE = Short-term (2008) displacements Long-term (1992-2010) displacements = Map representing an estimate of the present anthropogenic land movements at Venice (+ ; )
OBSERVED MOVEMENTS: WHICH THE CAUSES? Architecture of the shallow subsoil of Venice along the alignment A–D 1 : the heterogeneous nature of the Venice subsoil 2 : the city growth over the century Growth in area of Venice from 900 A.D. to present
OBSERVED MOVEMENTS: WHICH THE CAUSES? 3 : restoration works (e.g., building restoration, canal dredging, etc.) 4 : waves induced by the intensive boat and ship traffic Average displacement rates (mm/yr) obtained by PSI at a portion of the city NE of St. Mark’s Basilica where restoration works were carried out in 2008 Photos of the typical Venice traffic