LEADER 02321oam 2200385 450 001 9910774877603321 005 20230725053157.0 035 $a(CKB)3460000000088100 035 $a(NjHacI)993460000000088100 035 $a(EXLCZ)993460000000088100 100 $a20121230c2011uuuu uu 0 101 0 $aita 135 $auubu#---uu|uu 181 $ctxt$2rdacontent 182 $cn$2rdamedia 183 $anc$2rdacarrier 200 00$aAdvanced terrain mapping of the Gioia Tauro Plain Calabria Region, Italy $eESA GMES Terrafirma /$fedited by Federico Raspini, Francesca Cigna, Sandro Moretti, Nicola Casagli 210 1$aFirenze :$cFirenze University Press,$d2011 215 $a1 online resource (29 pages) $cillustrations, maps; digital, PDF file(s) 225 1 $aProceedings e report ;$v78 320 $aIncludes bibliographical references. 330 $aIn the framework of the Terrafirma project, Persistent Scatterers Interferometry (PSI) has be used for mapping land subsidence at basin scale in Gioia Tauro plain (Italy). The investigated area is built over unconsolidated fine-grained sediments, where the increasing groundwater demands for irrigation have caused the natural sediment consolidation to progressively accelerate. Both historical (1992-2001; ERS1/2 images) and recent (2002-2006; ENVISAT images) scenarios are analyzed to solve the spatial variability and temporal evolution of ground displacements affecting the plain. The results show deformation rates as high as 10-12 mm/yr in 1992-2007, with highest velocities occurred between 1992 and 2000 within the central part of the basin, in the area of Rizziconi (5 km ESE of Gioia Tauro). The outcomes of this PSI study could support the future improvement of groundwater management and the implementation of best strategies for land use planning and sustainable use of groundwater resources. 410 0$aProceedings e report ;$v78. 606 $aPhysical geology 615 0$aPhysical geology. 676 $a551 702 $aRaspini$b Federico 702 $aCigna$b Francesca 702 $aMoretti$b Sandro 702 $aCasagli$b Nicola 801 2$bUkMaJRU 906 $aBOOK 912 $a9910774877603321 996 $aAdvanced terrain mapping of the Gioia Tauro Plain Calabria Region, Italy$93662732 997 $aUNINA